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CN111610563B - A method and device for identifying multiple waves - Google Patents

A method and device for identifying multiple waves Download PDF

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CN111610563B
CN111610563B CN201910140962.XA CN201910140962A CN111610563B CN 111610563 B CN111610563 B CN 111610563B CN 201910140962 A CN201910140962 A CN 201910140962A CN 111610563 B CN111610563 B CN 111610563B
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reflectivity
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戴晓峰
甘利灯
贺维胜
邓志文
张旋
陈骁
陈康
张明
孙夕平
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Petrochina Co Ltd
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    • G01V1/00Seismology; Seismic or acoustic prospecting or detecting
    • G01V1/28Processing seismic data, e.g. for interpretation or for event detection
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Abstract

本发明提供一种识别多次波的方法和装置,该方法包括:获取地震工区的时间层位数据和测井数据;根据时间层位数据和测井数据,确定地震工区的波阻抗体;将波阻抗体转换为一次波反射率;根据一次波反射率和测井数据,正演合成一次波地震记录和全波地震记录;根据一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域。本发明能够对整个地震工区多次波的整体发育程度和分布情况进行预测,用于分析潜在多次波特征,应用在多次波压制处理中,从而实现多次波压制处理参数优选,一定程度上减少了压制多次波的不确定性;还能用于评价地震资料品质,划分出地震资料不可靠的区域,从而减小储层预测的多解性,降低井位部署的风险。

Figure 201910140962

The present invention provides a method and device for identifying multiple waves. The method includes: acquiring time horizon data and well logging data of the seismic work area; determining the wave impedance body of the seismic work area according to the time horizon data and well logging data; The acoustic impedance volume is converted into primary wave reflectivity; based on the primary wave reflectivity and logging data, the primary wave seismic record and the full wave seismic record are synthesized by forward modeling; according to the primary wave seismic record and the full wave seismic record, different The multiple interference area of the interference level. The present invention can predict the overall development degree and distribution of multiple waves in the entire seismic work area, which is used to analyze the characteristics of potential multiple waves, and is applied in multiple wave suppression processing, so as to realize the optimization of multiple wave suppression processing parameters, to a certain extent In addition, it reduces the uncertainty of suppressing multiple waves; it can also be used to evaluate the quality of seismic data and divide unreliable areas of seismic data, thereby reducing the multi-solution of reservoir prediction and reducing the risk of well location deployment.

Figure 201910140962

Description

一种识别多次波的方法和装置A method and device for identifying multiple waves

技术领域technical field

本发明属于石油勘探开发技术领域,尤其涉及一种识别多次波的方法和装置。The invention belongs to the technical field of petroleum exploration and development, in particular to a method and device for identifying multiple waves.

背景技术Background technique

在石油勘探中,地震波通过地下岩层传播,当遇到强反射界面时,则产生强能量的反射波。反射波返回向上传播遇到良好的强反射界面时,再次反射并向下传播,如此往返就形成了多次波。因此通常情况下,我国各个探区都不同程度地存在多次波,特别是在诸如四川盆地、塔里木盆地和鄂尔多斯盆地,构造平缓、强反射界面较多,多次波干扰更为严重。这类多次波与深层一次波振幅相当,动校正时差较小,与深层一次波相干涉,难以识别,影响地震数据偏移质量、地震属性提取以及反演等地震解释研究的可靠性。In oil exploration, seismic waves propagate through underground rock formations, and when encountering strong reflection interfaces, strong energy reflection waves are generated. When the reflected wave travels back upwards and encounters a good strong reflection interface, it is reflected again and propagates downwards, thus forming multiple waves back and forth. Therefore, under normal circumstances, multiple waves exist to varying degrees in various exploration areas in my country, especially in the Sichuan Basin, Tarim Basin, and Ordos Basin, where the structure is gentle and there are many strong reflection interfaces, and the multiple wave interference is more serious. This type of multiple wave has the same amplitude as the deep primary wave, and the dynamic correction time difference is small. It interferes with the deep primary wave and is difficult to identify, which affects the reliability of seismic interpretation research such as seismic data migration quality, seismic attribute extraction, and inversion.

由于多次波成因复杂,在地震资料处理过程中识别和压制难度大,会造成有效波反射能量畸变、使储层预测结果错误,给油气勘探和开发带来很大的风险,因此,有必要对其分布进行识别。Due to the complex causes of multiple waves, it is difficult to identify and suppress them in the process of seismic data processing, which will cause distortion of effective wave reflection energy, make reservoir prediction results wrong, and bring great risks to oil and gas exploration and development. Therefore, it is necessary to Identify its distribution.

目前地震处理解释中,通常基于多次波的速度和周期性特征在速度谱、叠加剖面、地震叠前道集上识别多次波:在叠前阶段,速度谱存在低速能量团、CMP道集上出现动校不足,随偏移距增大具有下拉现象、深层和浅层具有相似旅行周期;在叠后阶段,通过叠加地震剖面上强反射界面和强反射界面之下地震反射的形态和时间识别多次波;当地下反射界面倾角较小时,如果在强反射界面下方存在另一组与其形态一致,且出现时间小于其2倍的反射同相轴时,就可以判断该组同相轴为多次反射波;对于倾斜地层,叠加剖面上二次反射波的倾角约为其一次反射波的2倍。In current seismic processing and interpretation, multiples are usually identified on the velocity spectrum, stacked section, and seismic prestack gathers based on the velocity and periodicity of the multiples: in the prestack stage, there are low-velocity energy clusters and CMP gathers in the velocity spectrum. Insufficient dynamic correction occurs on the upper surface, and the pull-down phenomenon occurs with the increase of offset, and the deep layer and the shallow layer have similar travel periods; Identify multiple waves; when the inclination angle of the subterranean reflection interface is small, if there is another group of reflection events below the strong reflection interface that is consistent with its shape and whose appearance time is less than 2 times, it can be judged that this group of events is multiple Reflected waves; for inclined formations, the inclination angle of the secondary reflected waves on the stacked section is about twice that of the primary reflected waves.

但在现有技术中,都只能实现单个观测点(一个叠前地震道集或一个地震速度谱)和一条观测线(叠加地震剖面)上的多次波识别,无法得到多次波在地震工区平面上的整体发育程度和分布情况。由于地下构造和地层厚度变化很快,导致多次波在平面上也具有强烈的非均质特点,单个点和单条线的结果显然无法代表整个地震工区的情况,满足不了多次波识别和压制效果评价的需要。However, in the prior art, it is only possible to identify multiple waves on a single observation point (a pre-stack seismic gather or a seismic velocity spectrum) and an observation line (stacked seismic section), and it is impossible to obtain the The overall development degree and distribution on the plane of the work area. Due to the rapid change of the underground structure and stratum thickness, the multiple waves also have strong heterogeneity on the plane. The results of a single point and a single line obviously cannot represent the situation of the entire seismic work area, and cannot meet the requirements of multiple wave identification and suppression. The need for performance evaluation.

发明内容Contents of the invention

本发明实施例提供一种识别多次波的方法,利用反射率正演模拟方法得到多次波在某个地质层在平面上的能量分布,其结果可用于指导处理人员合理压制地震数据中存在的多次波,也可以用于解释人员评价地震资料品质,给储层预测结果进行可靠性评价,降低开发勘探中井位部署的风险,该方法包括:The embodiment of the present invention provides a method for identifying multiple waves, using the reflectivity forward modeling method to obtain the energy distribution of multiple waves in a certain geological layer on the plane, and the results can be used to guide the processing personnel to reasonably suppress the presence of multiple waves in seismic data. The multiple waves can also be used by interpreters to evaluate the quality of seismic data, evaluate the reliability of reservoir prediction results, and reduce the risk of well deployment in development and exploration. The method includes:

获取地震工区的时间层位数据和测井数据;Obtain the time horizon data and logging data of the seismic work area;

根据时间层位数据和测井数据,确定地震工区的波阻抗体;Determine the wave impedance volume of the seismic work area according to the time horizon data and logging data;

将波阻抗体转换为一次波反射率;Convert wave impedance volume to primary wave reflectivity;

根据一次波反射率和测井数据,正演合成一次波地震记录和全波地震记录;Based on the primary wave reflectivity and logging data, forward synthetic primary wave seismic records and full wave seismic records;

根据一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域。According to primary wave seismic records and full wave seismic records, multiple wave interference areas with different interference levels are determined from the seismic work area.

本发明实施例还提供一种识别多次波的装置,包括:The embodiment of the present invention also provides a device for identifying multiple waves, including:

数据获取模块,用于获取地震工区的时间层位数据和测井数据;The data acquisition module is used to acquire the time horizon data and logging data of the seismic work area;

波阻抗体确定模块,用于根据时间层位数据和测井数据,确定地震工区的波阻抗体;The acoustic impedance volume determination module is used to determine the acoustic impedance volume of the seismic work area according to the time horizon data and well logging data;

一次波反射率转换模块,用于将波阻抗体转换为一次波反射率;The primary wave reflectivity conversion module is used to convert the wave impedance body into the primary wave reflectivity;

正演合成模块,用于根据一次波反射率和测井数据,正演合成一次波地震记录和全波地震记录;The forward modeling synthesis module is used for forward modeling and synthesizing primary wave seismic records and full wave seismic records according to the primary wave reflectivity and logging data;

多次波干扰区域确定模块,用于根据一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域。The multiple wave interference area determination module is used to determine multiple wave interference areas of different interference levels from the seismic work area according to the primary wave seismic records and the full wave seismic records.

本发明实施例还提供一种计算机设备,包括存储器、处理器及存储在存储器上并可在处理器上运行的计算机程序,所述处理器执行所述计算机程序时实现上述识别多次波的方法。An embodiment of the present invention also provides a computer device, including a memory, a processor, and a computer program stored on the memory and operable on the processor, when the processor executes the computer program, the above-mentioned method for identifying multiple waves is realized .

本发明实施例还提供一种计算机可读存储介质,所述计算机可读存储介质存储有执行实现上述识别多次波的方法的计算机程序。An embodiment of the present invention also provides a computer-readable storage medium, where the computer-readable storage medium stores a computer program for implementing the above-mentioned method for identifying multiple waves.

本发明实施例提供的一种识别多次波的方法和装置,通过建立波阻抗体,利用反射率正演模拟的方法正演合成一次波地震记录和全波地震记录;通过对全波地震记录和一次波地震记录分析,得到多次波在某个地质层在平面上的能量分布,相对现有技术中多次波单点、单线的识别方法,本发明实施例能够对整个地震工区多次波的整体发育程度和分布情况进行预测,用于分析潜在多次波特征,应用在多次波压制处理中,从而实现多次波压制处理参数优选,一定程度上减少了压制多次波的不确定性;本发明实施例还能够根据划分的不同干扰等级多次波干扰区域,评价地震资料品质,划分出地震资料不可靠的区域,从而减小储层预测的多解性,降低井位部署的风险。The embodiment of the present invention provides a method and device for identifying multiple waves. By establishing an acoustic impedance volume, the reflectivity forward modeling method is used to forward synthesize primary wave seismic records and full-wave seismic records; through the full-wave seismic records The energy distribution of the multiple waves in a certain geological layer on the plane is obtained by analyzing the primary wave seismic records. Compared with the identification method of multiple wave single point and single line in the prior art, the embodiment of the present invention can multiple times for the entire seismic work area. It is used to predict the overall development degree and distribution of multiple waves, which is used to analyze the characteristics of potential multiple waves, and is applied in multiple wave suppression processing, so as to realize the optimization of multiple wave suppression processing parameters, and to a certain extent reduce the inconsistency of suppressing multiple waves. Certainty; the embodiment of the present invention can also evaluate the quality of seismic data according to the multiple interference areas of different interference levels, and divide the unreliable areas of seismic data, thereby reducing the ambiguity of reservoir prediction and reducing the deployment of well locations risks of.

附图说明Description of drawings

为了更清楚地说明本发明实施例或现有技术中的技术方案,下面将对实施例或现有技术描述中所需要使用的附图作简单地介绍,显而易见地,下面描述中的附图仅仅是本发明的一些实施例,对于本领域普通技术人员来讲,在不付出创造性劳动的前提下,还可以根据这些附图获得其他的附图。在附图中:In order to more clearly illustrate the technical solutions in the embodiments of the present invention or the prior art, the following will briefly introduce the drawings that need to be used in the description of the embodiments or the prior art. Obviously, the accompanying drawings in the following description are only These are some embodiments of the present invention. Those skilled in the art can also obtain other drawings based on these drawings without creative work. In the attached picture:

图1为本发明实施例一种识别多次波的方法的示意图。FIG. 1 is a schematic diagram of a method for identifying multiples according to an embodiment of the present invention.

图2为本发明实施例一种识别多次波的方法的应用实例建立的波阻抗体在某条地震测线上显示的结果示意图。Fig. 2 is a schematic diagram showing the results displayed on a certain seismic survey line by an acoustic impedance body established by an application example of a method for identifying multiples according to an embodiment of the present invention.

图3为本发明实施例一种识别多次波的方法的应用实例的一次波地震记录地震剖面图。Fig. 3 is a seismic section view of a primary wave seismic record of an application example of a method for identifying multiples according to an embodiment of the present invention.

图4为本发明实施例一种识别多次波的方法的确定全波反射率的流程图。Fig. 4 is a flow chart of determining the total wave reflectivity of a method for identifying multiple waves according to an embodiment of the present invention.

图5为本发明实施例一种识别多次波的方法的应用实例的全波地震记录地震剖面图。Fig. 5 is a seismic section view of a full-wave seismic record of an application example of a method for identifying multiple waves according to an embodiment of the present invention.

图6为本发明实施例一种识别多次波的方法的应用实例中相同位置的多次波地震记录图。Fig. 6 is a multiple wave seismogram at the same location in an application example of a method for identifying multiple waves according to an embodiment of the present invention.

图7为本发明实施例一种识别多次波的方法的应用实例获取的信噪比属性切片图。FIG. 7 is a SNR attribute slice diagram obtained by an application example of a method for identifying multiples according to an embodiment of the present invention.

图8为本发明实施例一种识别多次波的装置示意图。FIG. 8 is a schematic diagram of an apparatus for identifying multiple waves according to an embodiment of the present invention.

具体实施方式Detailed ways

为使本发明实施例的目的、技术方案和优点更加清楚明白,下面结合附图对本发明实施例做进一步详细说明。在此,本发明的示意性实施例及其说明用于解释本发明,但并不作为对本发明的限定。In order to make the purpose, technical solutions and advantages of the embodiments of the present invention more clear, the embodiments of the present invention will be further described in detail below in conjunction with the accompanying drawings. Here, the exemplary embodiments and descriptions of the present invention are used to explain the present invention, but not to limit the present invention.

本发明实施例提供一种识别多次波的方法,利用反射率正演模拟方法得到多次波在某个地质层在平面上的能量分布,其结果可用于指导处理人员合理压制地震数据中存在的多次波,也可以用于解释人员评价地震资料品质,给储层预测结果进行可靠性评价,降低开发勘探中井位部署的风险,如图1本发明实施例一种识别多次波的方法的示意图所示,该方法包括:The embodiment of the present invention provides a method for identifying multiple waves, using the reflectivity forward modeling method to obtain the energy distribution of multiple waves in a certain geological layer on the plane, and the results can be used to guide the processing personnel to reasonably suppress the presence of multiple waves in seismic data. The multiple waves can also be used for interpreters to evaluate the quality of seismic data, to evaluate the reliability of reservoir prediction results, and to reduce the risk of well location deployment in development and exploration, as shown in Figure 1. A method for identifying multiple waves in an embodiment of the present invention As shown in the schematic diagram of , the method includes:

步骤101,获取地震工区的时间层位数据和测井数据;Step 101, obtaining time horizon data and logging data of the seismic work area;

步骤102,根据时间层位数据和测井数据,确定地震工区的波阻抗体;Step 102, according to the time horizon data and logging data, determine the wave impedance volume of the seismic work area;

步骤103,将波阻抗体转换为一次波反射率;Step 103, converting the wave impedance volume into primary wave reflectivity;

步骤104,根据一次波反射率和测井数据,正演合成一次波地震记录和全波地震记录;Step 104, according to the reflectivity of the primary wave and the logging data, forward modeling synthesizes the primary wave seismic record and the full wave seismic record;

步骤105,根据一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域。Step 105, according to the primary wave seismic records and the full wave seismic records, multiple wave interference areas of different interference levels are determined from the seismic work area.

本发明实施例能够对整个地震工区多次波的整体发育程度和分布情况进行预测,用于分析潜在多次波特征,应用在多次波压制处理中,从而实现多次波压制处理参数优选,一定程度上减少了压制多次波的不确定性;本发明实施例还能够根据划分的不同干扰等级多次波干扰区域,评价地震资料品质,划分出地震资料不可靠的区域,从而减小储层预测的多解性,降低井位部署的风险。The embodiment of the present invention can predict the overall development degree and distribution of multiples in the entire seismic work area, which is used to analyze the characteristics of potential multiples, and is applied in the processing of multiples suppression, thereby realizing the optimization of processing parameters for multiples suppression. To a certain extent, the uncertainty of suppressing multiple waves is reduced; the embodiment of the present invention can also evaluate the quality of seismic data according to the divided multiple wave interference areas of different interference levels, and divide the unreliable areas of seismic data, thereby reducing the storage capacity. The multi-solution of layer prediction reduces the risk of well location deployment.

在具体实施多次波识别方法的时候,首先需要获取地震工区的时间层位数据和测井数据;然后根据时间层位数据和测井数据,确定地震工区的波阻抗体;随后将波阻抗体转换为一次波反射率;再根据一次波反射率和测井数据,正演合成一次波地震记录和全波地震记录;最后,根据正演合成的一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域。When implementing the multiple wave identification method, it is first necessary to obtain the time horizon data and logging data of the seismic work area; then determine the acoustic impedance volume of the seismic work area according to the time horizon data and well logging data; converted into primary wave reflectivity; then based on the primary wave reflectivity and logging data, forward synthetic primary wave seismic records and full wave seismic records; finally, based on the forward modeling synthetic primary wave seismic records and full wave seismic records, the Determine the multiple wave interference areas with different interference levels in the work area.

本发明实施例提供一采用多次波识别方法的应用实例:在四川盆地川中地区某三维地震工区的深层震旦系灯四段,发现了高产、富集的碳酸盐岩岩溶气藏。川中地区已钻井揭示,深层灯影组地层之上中、浅层存在多个反射界面;四川盆地从晚三叠世至新生代为海陆交互相沉积的砂泥岩地层为主,从震旦纪至中三叠世为海相碳酸盐岩台地沉积的碳酸盐岩地层;砂泥岩到碳酸盐岩地层岩性的转变,形成了区域良好的波阻抗反射界面;由于强反射界面数量多、纵向时间构造存在一定的变化,导致在强反射界面之下特别是在灯影组内部产生了复杂的多次波干扰;这些层间多次波来源多、成因复杂,其速度和一次波的速度差异小,因此地震数据中难以对一次有效波和多次波进行有效区分和识别,给地震处理带来很大的困扰,难以得到高信噪比的地震成果资料;因此在该地震工区可以应用本发明实施例提供的识别多次波的方法,实现多次波的有效识别。The embodiment of the present invention provides an application example of using the multiple wave identification method: in the deep Sinian Deng 4 member in a 3D seismic work area in the central Sichuan Basin, a high-yield and enriched carbonate rock karst gas reservoir was discovered. Drilling in the central Sichuan area has revealed that there are multiple reflection interfaces in the middle and shallow layers above the deep Dengying Formation; the Sichuan Basin is dominated by sandstone and mudstone strata deposited in marine-terrestrial interactions from the Late Triassic to the Cenozoic, and from the Sinian to the Middle Triassic. The superimposed carbonate rock strata were deposited on marine carbonate rock platforms; the lithology transition from sandy mudstone to carbonate rock strata formed a good wave impedance reflection interface in the region; due to the large number of strong reflection There are certain changes in the structure, which lead to complex multiple wave interference under the strong reflection interface, especially in the Dengying Formation; these interlayer multiple waves have many sources and complex causes, and the difference between the velocity and the velocity of the primary wave is small. Therefore, it is difficult to effectively distinguish and identify primary effective waves and multiple waves in seismic data, which brings great troubles to seismic processing, and it is difficult to obtain seismic result data with high signal-to-noise ratio; therefore, the present invention can be applied in this seismic work area. The method of identifying multiple waves provided by the example realizes the effective identification of multiple waves.

具体实施获取地震工区的时间层位数据和测井数据时,在一个实施例中,测井数据可以包括波阻抗曲线;根据时间层位数据和测井数据,确定地震工区的波阻抗体,具体可以包括:以时间层位数据为约束,利用反距离插值算法,对波阻抗曲线进行三维空间插值,确定波阻抗体。When specifically implementing the time horizon data and logging data of the seismic work area, in one embodiment, the well logging data can include wave impedance curves; according to the time horizon data and well logging data, determine the wave impedance volume of the seismic work area, specifically It may include: taking the time horizon data as constraints, and using the inverse distance interpolation algorithm to perform three-dimensional space interpolation on the wave impedance curve to determine the wave impedance volume.

在本发明实施例的应用实例中,从油田、地球物理服务公司等处获取地震工区的时间层位数据,从浅到深包括上三叠系须家河(T3x1)、下三叠系飞4段(T1f4)、上二叠系长兴组(P2ch)、龙潭组(P2l)和下二叠系梁山组(P1l)、奥陶系(O)、寒武系龙王庙组

Figure BDA0001978522100000052
寒武系筇竹寺组
Figure BDA0001978522100000053
震旦系灯三段(Z2d3)和灯影组(Z2d)等底界的10个时间层位数据。In the application example of the embodiment of the present invention, the time horizon data of the seismic work area are obtained from oil fields, geophysical service companies, etc., including the Upper Triassic Xujiahe (T 3 x1), Lower Triassic Fei 4 Member (T 1 f4), Upper Permian Changxing Formation (P 2 ch), Longtan Formation (P 2 l), Lower Permian Liangshan Formation (P 1 l), Ordovician (O), Cambrian Longwangmiao Formation
Figure BDA0001978522100000052
Cambrian Qiongzhusi Formation
Figure BDA0001978522100000053
Data of 10 time horizons of the lower boundary of the third member of the Dengying Formation (Z 2 d3) and the Dengying Formation (Z 2 d) of the Sinian system.

在获取到地震工区的时间层位数据和测井数据后,利用地震反演解释软件的建立初始模型模块,以时间层位为约束,对波阻抗曲线进行空间插值,创建波阻抗体,具体可以为:将上述获取到的地震工区的时间层位数据导入Jason软件Earth Model建模模块中,联合测井数据中的波阻抗曲线,在上述10个时间层位数据的约束下,利用反距离插值算法,对波阻抗曲线进行三维空间插值,建立波阻抗体。图2为本发明实施例一种识别多次波的方法的应用实例建立的波阻抗体在某条地震测线上显示的结果示意图,图2中还同时显示了前述的时间层位数据。After obtaining the time horizon data and logging data of the seismic work area, use the seismic inversion interpretation software to establish the initial model module, and use the time horizon as a constraint to perform spatial interpolation on the wave impedance curve to create a wave impedance volume. To: import the time horizon data of the seismic work area obtained above into the Earth Model modeling module of Jason software, and the wave impedance curve in the joint logging data, under the constraints of the above 10 time horizon data, use inverse distance interpolation Algorithm, perform three-dimensional space interpolation on the wave impedance curve, and establish the wave impedance volume. Fig. 2 is a schematic diagram of the results displayed on a certain seismic survey line by an acoustic impedance volume established by an application example of a method for identifying multiples according to an embodiment of the present invention. Fig. 2 also shows the aforementioned time horizon data at the same time.

在建立波阻抗体后,再将波阻抗体转化为一次波反射率;具体实施时,在一个实施例中,可以按照如下方式,将波阻抗体转换为一次波反射率:After the wave impedance body is established, the wave impedance body is converted into the primary wave reflectivity; during specific implementation, in one embodiment, the wave impedance body can be converted into the primary wave reflectivity in the following manner:

Figure BDA0001978522100000051
Figure BDA0001978522100000051

其中,r为一次波反射率;PI为波阻抗体;i为反射率采样点序号。Among them, r is the reflectivity of the primary wave; PI is the wave impedance body; i is the serial number of the reflectivity sampling point.

前述提到的将波阻抗体转换为一次波反射率的表达式为举例说明,本领域技术人员可以理解,在实施时还可以根据需要对上述公式进行一定形式的变形和添加其它的参数或数据,或者提供其它的具体公式,这些变化例均应落入本发明的保护范围。The above-mentioned expression for converting the wave impedance body into the primary wave reflectivity is an example, and those skilled in the art can understand that the above formula can also be deformed in a certain form and other parameters or data can be added according to the needs during implementation. , or provide other specific formulas, these variations should fall within the protection scope of the present invention.

在将波阻抗体转换为一次波反射率后,在一个实施例中,可以采用反射率正演模拟的方法,根据一次波反射率和测井数据,正演合成一次波地震记录和全波地震记录,测井数据可以包括地震子波。其中,根据一次波反射率和测井数据,正演合成一次波地震记录,可以包括:将一次波反射率和地震子波进行褶积计算,正演合成一次波地震记录。在具体实施时,可以按照如下方式,正演合成一次波地震记录:After converting the acoustic impedance volume into the primary wave reflectivity, in one embodiment, the reflectivity forward modeling method can be used to forward synthesize primary wave seismic records and full-wave seismic data according to the primary wave reflectivity and logging data. Recorded, well log data may include seismic wavelets. Wherein, the forward modeling and synthesizing the primary seismic records according to the primary reflectivity and logging data may include: performing convolution calculation on the primary reflectivity and the seismic wavelet, and forward synthesizing the primary seismic records. In specific implementation, the forward modeling of synthetic primary seismic records can be carried out in the following manner:

Figure BDA0001978522100000061
Figure BDA0001978522100000061

其中,Sy为一次波地震记录;w为地震子波;r为一次波反射率;i为反射率采样点序号;N为地震子波长度;j为地震子波采样点序号。Among them, Sy is the seismic record of the primary wave; w is the seismic wavelet; r is the reflectivity of the primary wave; i is the serial number of the reflectivity sampling point; N is the length of the seismic wavelet; j is the serial number of the seismic wavelet sampling point.

前述提到的正演合成一次波地震记录的表达式为举例说明,本领域技术人员可以理解,在实施时还可以根据需要对上述公式进行一定形式的变形和添加其它的参数或数据,或者提供其它的具体公式,这些变化例均应落入本发明的保护范围。The expression of the above-mentioned forward modeling synthetic primary wave seismic record is an example, and those skilled in the art can understand that the above formula can also be deformed in a certain form and add other parameters or data according to the needs during implementation, or provide Other specific formulas and these variation examples should all fall within the protection scope of the present invention.

在本发明实施例的应用实例中,分析实际地震资料的主频为32Hz,因此选取32Hz的雷克子波为地震子波进行正演。图3为本发明实施例一种识别多次波的方法的应用实例的一次波地震记录地震剖面图。由图3可见,一次波反射率和32Hz雷克子波褶积得到的一次波地震记录地震剖面图,理论一次波的地震反射横向连续性好,纵向上强弱对比明显,深层

Figure BDA0001978522100000062
Z2d3等3个界面强反射界面清晰。In the application example of the embodiment of the present invention, the main frequency for analyzing the actual seismic data is 32 Hz, so the 32 Hz Lake wavelet is selected as the seismic wavelet for forward modeling. Fig. 3 is a seismic section view of a primary wave seismic record of an application example of a method for identifying multiples according to an embodiment of the present invention. It can be seen from Fig. 3 that the seismic profile of the primary wave seismic record obtained by the convolution of the primary wave reflectivity and the 32Hz Reckon wavelet shows that the seismic reflection of the theoretical primary wave has good lateral continuity, and the vertical strength contrast is obvious.
Figure BDA0001978522100000062
The three interfaces such as Z 2 d3 have clear strong reflection interfaces.

在正演合成一次波地震记录后,接着正演合成全波地震记录;在一个实施例中,根据一次波反射率和测井数据,正演合成全波地震记录,可以包括:根据一次波反射率,确定全波反射率,将全波反射率和地震子波进行褶积计算,正演合成全波地震记录。在具体实施根据一次波反射率确定全波反射率时,可以输入一次波反射率(r)及其采样点数(M),按照图4本发明实施例一种识别多次波的方法的确定全波反射率的流程图所示,计算得到全波反射率(r'):After forward modeling and synthesizing the primary wave seismic records, then forward modeling and synthesizing the full wave seismic records; in one embodiment, according to the primary wave reflectivity and logging data, forward modeling and synthesizing the full wave seismic records may include: rate, determine the full-wave reflectivity, perform convolution calculation on the full-wave reflectivity and seismic wavelet, and synthesize full-wave seismic records by forward modeling. When determining the full-wave reflectivity according to the primary-wave reflectivity in specific implementation, the primary-wave reflectivity (r) and its number of sampling points (M) can be input, and the determination of the full-wave reflectance of a method for identifying multiple waves according to the embodiment of the present invention in FIG. 4 As shown in the flow chart of wave reflectivity, the total wave reflectivity (r') is calculated as:

首先通过i=0,dw0=1设置起始点时间为0,初始下行波能量为1,通过up=0,j=i设置初始上行波能量为0,然后根据dwj+1=-rj*up+(1-rj)*dwj计算j时间的下行反射波,根据up=rj*dwj+(1+rj)*up计算j时间的上行反射波,接着从时间i~0循环迭代,直至j<0,再然后通过dw0=0,i=i+1设置初始下行波能量为0,通过r'i=up得到i时间的反射波能量,再接着进行从时间0~M循环迭代,直至i>M-1,最终输出r',得到全波反射率。First, set the starting point time to 0 by i=0, dw 0 =1, and the initial downgoing wave energy to 1, and set up=0, j=i to set the initial upgoing wave energy to 0, and then according to dw j+1 = -r j *up+(1-r j )*dw j calculates the downgoing reflected wave at time j, and calculates the upgoing reflected wave at time j according to up=r j *dw j +(1+r j )*up, and then from time i to 0 Loop iteratively until j<0, then set the initial downgoing wave energy to 0 through dw 0 =0, i=i+1, get the reflected wave energy at time i through r' i =up, and then proceed from time 0 to M cycle iterates until i>M-1, and finally outputs r' to obtain the full-wave reflectivity.

其中,r为一次波反射率;M为一次波反射率采样点数;r'为全波反射率;up为上行波;dw为行波。Among them, r is the reflectivity of the primary wave; M is the number of sampling points of the reflectivity of the primary wave; r' is the reflectivity of the total wave; up is the upward wave; dw is the traveling wave.

在上述计算得到全波反射率的过程中,涉及的公式和表达式为举例说明,本领域技术人员可以理解,在实施时还可以根据需要对上述公式和表达式进行一定形式的变形和添加其它的参数或数据,或者提供其它的具体公式,这些变化例均应落入本发明的保护范围。In the process of calculating the full-wave reflectivity above, the formulas and expressions involved are examples, and those skilled in the art can understand that the above formulas and expressions can also be modified in a certain form and added other Parameters or data, or provide other specific formulas, these variations should fall within the protection scope of the present invention.

在确定全波反射率后,正演合成全波地震记录。在一个实施例中,具体实施正演合成全波地震记录时,将全波反射率和地震子波进行褶积计算,正演合成全波地震记录;进一步的,可以按如下方式,正演合成全波地震记录:After determining the full-wave reflectivity, the synthetic full-wave seismic record is forward modeled. In one embodiment, when implementing forward modeling and synthesizing full-wave seismic records, the full-wave reflectivity and seismic wavelets are convoluted to perform forward modeling and synthesizing full-wave seismic records; further, the forward modeling and synthesis can be performed as follows Full-wave seismic records:

Figure BDA0001978522100000071
Figure BDA0001978522100000071

其中,Sy'为全波地震记录;w为地震子波;r'为全波反射率;i为反射率采样点序号;N为地震子波长度,j为地震子波采样点序号。Among them, Sy' is the full-wave seismic record; w is the seismic wavelet; r' is the full-wave reflectivity; i is the reflectivity sampling point number; N is the seismic wavelet length, and j is the seismic wavelet sampling point number.

前述提到的正演合成全波地震记录的表达式为举例说明,本领域技术人员可以理解,在实施时还可以根据需要对上述公式进行一定形式的变形和添加其它的参数或数据,或者提供其它的具体公式,这些变化例均应落入本发明的保护范围。The expression of the above-mentioned forward synthetic full-wave seismic record is an example, and those skilled in the art can understand that the above-mentioned formula can also be deformed in a certain form and add other parameters or data according to the needs during implementation, or provide Other specific formulas and these variation examples should all fall within the protection scope of the present invention.

在本发明前述应用实例中,与正演合成一次地震波记录相似的,选取相同的32Hz雷克子波作为地震子波,与全波反射率进行褶积计算得到全波地震记录,图5为本发明实施例一种识别多次波的方法的应用实例的全波地震记录地震剖面图,由图5可见,全波反射率和32Hz雷克子波褶积得到的全波地震记录地震剖面图,考虑了下行反射后,地震剖面中除了一次反射还包含了多次波反射,相对一次波合成地震剖面,全波合成地震剖面整体信噪比降低、连续性变差;受多次波的干扰影响,深层

Figure BDA0001978522100000072
Figure BDA0001978522100000073
Z2d3等3个界面强反射均明显受到不同程度的减弱,Z2d3反射整体变得不易识别,图5地震剖面图左侧的
Figure BDA0001978522100000074
强反射严重被屏蔽变为弱反射;通过对比图5和图3的正演合成地震剖面图,可以清晰地看出多次波在深层灯影组的发育程度和对地震反射振幅的影响程度。In the aforementioned application example of the present invention, similar to the forward modeling and synthesis of a seismic wave record, the same 32Hz Reich wavelet is selected as the seismic wavelet, and is convoluted with the full-wave reflectivity to obtain a full-wave seismic record. Figure 5 is a graph of the present invention Embodiment A full-wave seismic record seismic profile of an application example of a method for identifying multiple waves, as seen in Figure 5, the full-wave seismic record seismic profile obtained by full-wave reflectivity and 32Hz Reckont wavelet convolution, considering After the down-going reflection, the seismic section includes multiple reflections in addition to the primary reflection. Compared with the primary-wave synthetic seismic section, the overall signal-to-noise ratio of the full-wave synthetic seismic section decreases and the continuity becomes poor; affected by the interference of multiple waves, the deep layer
Figure BDA0001978522100000072
Figure BDA0001978522100000073
The strong reflections at the three interfaces such as Z 2 d3 are obviously weakened to varying degrees, and the overall reflection of Z 2 d3 becomes difficult to identify. The left side of the seismic section in Figure 5
Figure BDA0001978522100000074
Strong reflections were severely shielded and turned into weak reflections; by comparing the forward modeling seismic profiles in Figure 5 and Figure 3, we can clearly see the degree of development of multiple waves in the deep Dengying Formation and the degree of influence on seismic reflection amplitude.

在正演合成一次波地震记录和全波地震记录后,根据一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域;在一个实施例中,具体实施根据一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域时,可以包括:根据一次波地震记录和全波地震记录,确定多次波地震记录;根据一次波地震记录和多次波地震记录,确定信噪比属性切片;根据信噪比属性切片,从地震工区中确定不同干扰等级的多次波干扰区域。After the primary and full-wave seismic records are synthesized by forward modeling, the multiple-wave interference areas of different interference levels are determined from the seismic work area according to the primary-wave seismic records and the full-wave seismic records; in one embodiment, the specific implementation is based on When primary wave seismic records and full wave seismic records are used to determine multiple wave interference areas of different interference levels from the seismic work area, it may include: determining multiple wave seismic records based on primary wave seismic records and full wave seismic records; Seismic records and multiple seismic records, determine the SNR attribute slice; determine the multiple wave interference area with different interference levels from the seismic work area according to the SNR attribute slice.

其中,根据一次波地震记录和全波地震记录,确定多次波地震记录,在一个实施例中,可以包括:将全波地震记录减去一次波地震记录,得到多次波地震记录;具体实施时,可以按照如下方式,确定多次波地震记录:Wherein, according to the primary wave seismic record and the full wave seismic record, determining the multiple wave seismic record may include: subtracting the full wave seismic record from the primary wave seismic record to obtain the multiple wave seismic record; , the multiple seismic records can be determined as follows:

ΔSy=Sy'-SyΔSy=Sy'-Sy

其中:ΔSy为多次波地震记录;Sy'为全波地震记录;Sy为一次波地震记录。Among them: ΔSy is the multiple wave seismic record; Sy' is the full wave seismic record; Sy is the primary wave seismic record.

前述提到的确定多次波地震记录的表达式为举例说明,本领域技术人员可以理解,在实施时还可以根据需要对上述公式进行一定形式的变形和添加其它的参数或数据,或者提供其它的具体公式,这些变化例均应落入本发明的保护范围。The above-mentioned expressions for determining multiple seismic records are examples, and those skilled in the art can understand that the above-mentioned formulas can also be modified in a certain form and added with other parameters or data according to needs, or other parameters can be provided. The specific formulas, these variations all should fall within the scope of protection of the present invention.

图6为本发明实施例一种识别多次波的方法的应用实例中相同位置的多次波地震记录图,如图6所示,可以更加清楚地看出多次波能量在不同时间层位能量有所变化,特别是强能量多次波主要出现在寒武系筇竹寺组

Figure BDA0001978522100000081
至震旦系灯三段(Z2d3)之间的灯四段气藏上,并且横向上强度也有所差异,会对地震储层预测结果造成较大的影响。Fig. 6 is a multiple wave seismogram at the same position in an application example of a method for identifying multiple waves in an embodiment of the present invention. As shown in Fig. 6, it can be seen more clearly that multiple wave energy is in different time horizons The energy has changed, especially the strong energy multiples mainly appear in the Cambrian Qiongzhusi Formation
Figure BDA0001978522100000081
To the Deng 4 member gas reservoir between the Sinian Deng 3 member (Z2d3), and the strength is also different in the lateral direction, which will have a greater impact on the seismic reservoir prediction results.

在确定多次波地震记录后,根据一次波地震记录和多次波地震记录,确定信噪比属性切片;一个实施例中,在具体实施确定信噪比属性切片时,可以包括:对一次波地震记录(Sy)沿时间层位提取属性值,获得一次波沿层属性切片(At);对多次波地震记录(ΔSy)沿时间层位提取属性值,获得多次波沿层属性切片(ΔAt);根据一次波沿层属性切片(At)和多次波沿层属性切片(ΔAt),确定信噪比属性切片(SN)。进一步的,在具体实施提取属性值时,本领域技术人员可以理解的,可以采用如下任一种或多种组合的计算方法,包括:求取均方根值计算、最大值计算、正值平均计算、波谷平均计算、振幅绝对值计算、能量求取计算等常规地震属性计算。After determining the multiple seismic records, determine the SNR attribute slice according to the primary seismic records and the multiple seismic records; in one embodiment, when determining the SNR attribute slice in specific implementation, it may include: Seismic records (Sy) extract attribute values along time horizons to obtain primary wave attribute slices (At); for multiple seismic records (ΔSy) to extract attribute values along time horizons, multiple wave along layer attribute slices ( ΔAt); determine the signal-to-noise ratio attribute slice (SN) according to the primary wave along-layer attribute slice (At) and the multiple wave along-layer attribute slice (ΔAt). Further, when extracting attribute values, those skilled in the art can understand that any one or more of the following calculation methods can be used, including: root mean square value calculation, maximum value calculation, positive value average Calculation, trough average calculation, amplitude absolute value calculation, energy calculation and other conventional seismic attribute calculations.

在确定了一次波沿层属性切片和多次波沿层属性切片后,再确定信噪比属性切片;在一个实施中,具体实施确定信噪比属性切片时,可以包括:将一次波沿层属性切片(At)与多次波沿层属性切片(ΔAt)的比值确定为信噪比属性切片(SN)。After determining the slice of the primary wave along the layer attribute and the slice of the multiple wave along the layer attribute, then determine the slice of the SNR attribute; in one implementation, when determining the slice of the SNR attribute, it may include: The ratio of the attribute slice (At) to the multiple wave along-layer attribute slice (ΔAt) is determined as the signal-to-noise ratio attribute slice (SN).

在确定了信噪比属性切片后,根据信噪比属性切片,从地震工区中确定不同干扰等级的多次波干扰区域;在具体实施从地震工区中确定不同干扰等级的多次波干扰区域时,在一个实施例中,从地震工区中确定不同干扰等级的多次波干扰区域可以包括:After determining the SNR attribute slice, according to the SNR attribute slice, determine the multiple wave interference area with different interference levels from the seismic work area; when determining the multiple wave interference area with different interference levels in the seismic work area , in one embodiment, determining the multiple wave interference areas of different interference levels from the seismic work area may include:

将信噪比属性切片的值大于2的多次波干扰区域,确定为地震工区中第一干扰等级的多次波干扰区域;The multiple wave interference area where the value of the SNR attribute slice is greater than 2 is determined as the multiple wave interference area of the first interference level in the seismic work area;

将信噪比属性切片的值大于1小于2的多次波干扰区域,确定为地震工区中第二干扰等级的多次波干扰区域;The multiple wave interference area with the value of the signal-to-noise ratio attribute slice greater than 1 and less than 2 is determined as the multiple wave interference area of the second interference level in the seismic work area;

将信噪比属性切片的值小于1的多次波干扰区域,确定为地震工区中第三干扰等级的多次波干扰区域;The multiple wave interference area where the value of the SNR attribute slice is less than 1 is determined as the third interference level multiple wave interference area in the seismic work area;

其中,第一干扰等级小于第二干扰等级,第二干扰等级小于第三干扰等级。Wherein, the first interference level is smaller than the second interference level, and the second interference level is smaller than the third interference level.

在划分的不同干扰等级的多次波干扰区域中,第一干扰等级的多次波干扰区域地震资料质量可信度高,地震反射能够有效反映储层的特征;第二干扰等级的多次波干扰区域地震资料可信度一般,干扰波接近有效波能量,利用地震预测储层具有较强的多解性;第三干扰等级的多次波干扰区域干扰波能量强于有效波,此时地震反射已不能有效反映出储层的特征。Among the divided multiple wave interference areas of different interference levels, the seismic data quality of the multiple wave interference area of the first interference level is high, and the seismic reflection can effectively reflect the characteristics of the reservoir; the multiple wave interference area of the second interference level The reliability of the seismic data in the interference area is general, the interference wave is close to the energy of the effective wave, and the use of earthquakes to predict the reservoir has strong multi-solution; the energy of the interference wave in the interference area of the third interference level is stronger than that of the effective wave. Reflection can no longer effectively reflect the characteristics of the reservoir.

在本发明实施例的应用实例中,图7为本发明实施例一种识别多次波的方法的应用实例获取的信噪比属性切片图,在图7中,第一干扰等级的多次波干扰区域划分为I类多次波弱干扰区,指示地震资料质量可信度高,地震反射能够有效反映储层的特征;第二干扰等级的多次波干扰区域划分为II类多次波中干扰区,指示地震资料可信度一般,干扰波接近有效波能量,利用地震预测储层具有较强的多解性;第三干扰等级的多次波干扰区域划分为III类多次波强干扰区,指示干扰波能量强于有效波,此时地震反射已不能有效反映出储层的特征。由于在本发明实施例的应用实例中,震旦系灯四段为主力气藏,因此,对寒武系筇竹寺组

Figure BDA0001978522100000091
至震旦系灯三段(Z2d3)两个时间层位之间的数据进行振幅均方根属性提取计算,最终获取了如图7所示的灯四段信噪比属性切片。如图7所示,在该三维地震工区,多次波干扰在空间上分布很不均匀,在主力含气层灯四段附近,强干扰主要位于工区北部,南部多次波干扰相对较弱,因此,在北部地区依靠地震进行井位部署具有较强的风险。In the application example of the embodiment of the present invention, FIG. 7 is a SNR attribute slice diagram obtained by an application example of a method for identifying multiples in the embodiment of the present invention. In FIG. 7 , the multiples of the first interference level The interference area is divided into Type I multiple wave weak interference area, which indicates that the quality of seismic data is high and the seismic reflection can effectively reflect the characteristics of the reservoir; the second interference level multiple wave interference area is divided into Type II multiple wave medium In the interference area, the reliability of seismic data is average, the interference wave is close to the effective wave energy, and the seismic prediction of reservoir has strong multi-solution; the third interference level multiple wave interference area is classified as III strong multiple wave interference area, indicating that the energy of the interference wave is stronger than that of the effective wave. At this time, the seismic reflection cannot effectively reflect the characteristics of the reservoir. Since in the application example of the embodiment of the present invention, the fourth member of the Sinian system is the main gas reservoir, therefore, for the Cambrian Qiongzhusi Formation
Figure BDA0001978522100000091
The data between the two time horizons of the third member of the Sinian system (Z2d3) were extracted and calculated for the root mean square attribute of the amplitude, and finally the SNR attribute slice of the fourth member of the Dengeng as shown in Figure 7 was obtained. As shown in Fig. 7, in the 3D seismic work area, the multiple wave interference is very unevenly distributed in space. Near the main gas-bearing layer Deng 4, the strong interference is mainly located in the north of the work area, and the multiple wave interference is relatively weak in the south. Therefore, relying on earthquakes for well deployment in the northern region has a strong risk.

本发明实施例还提供一种计算机设备,包括存储器、处理器及存储在存储器上并可在处理器上运行的计算机程序,所述处理器执行所述计算机程序时实现上述识别多次波的方法。An embodiment of the present invention also provides a computer device, including a memory, a processor, and a computer program stored on the memory and operable on the processor, when the processor executes the computer program, the above-mentioned method for identifying multiple waves is realized .

本发明实施例还提供一种计算机可读存储介质,所述计算机可读存储介质存储有执行实现上述识别多次波的方法的计算机程序。An embodiment of the present invention also provides a computer-readable storage medium, where the computer-readable storage medium stores a computer program for implementing the above-mentioned method for identifying multiple waves.

本发明实施例中还提供了一种识别多次波的装置,如下面的实施例所述。由于该装置解决问题的原理与一种识别多次波的方法相似,因此该装置的实施可以参见一种识别多次波的方法的实施,重复之处不再赘述。Embodiments of the present invention also provide a device for identifying multiple waves, as described in the following embodiments. Since the problem-solving principle of the device is similar to a method for identifying multiples, the implementation of the device can refer to the implementation of a method for identifying multiples, and the repetition will not be repeated.

图8是本发明实施例一种识别多次波的装置示意图,如图8所示,该装置可以包括:Fig. 8 is a schematic diagram of a device for identifying multiple waves according to an embodiment of the present invention. As shown in Fig. 8, the device may include:

数据获取模块801,用于获取地震工区的时间层位数据和测井数据;The data acquisition module 801 is used to acquire the time horizon data and logging data of the seismic work area;

波阻抗体确定模块802,用于根据时间层位数据和测井数据,确定地震工区的波阻抗体;The acoustic impedance volume determination module 802 is used to determine the acoustic impedance volume of the seismic work area according to the time horizon data and well logging data;

一次波反射率转换模块803,用于将波阻抗体转换为一次波反射率;The primary wave reflectivity conversion module 803 is used to convert the wave impedance volume into the primary wave reflectivity;

正演合成模块804,用于根据一次波反射率和测井数据,正演合成一次波地震记录和全波地震记录;The forward modeling synthesis module 804 is used for forward modeling and synthesizing primary wave seismic records and full wave seismic records according to the primary wave reflectivity and logging data;

多次波干扰区域确定模块805,用于根据一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域。The multiple wave interference area determination module 805 is used to determine multiple wave interference areas of different interference levels from the seismic work area according to the primary wave seismic records and the full wave seismic records.

一个实施例中,所述数据获取模块获取的测井数据包括波阻抗曲线;In one embodiment, the logging data acquired by the data acquisition module includes wave impedance curves;

波阻抗体确定模块根据时间层位数据和测井数据,确定地震工区的波阻抗体,包括:The acoustic impedance volume determination module determines the acoustic impedance volume of the seismic work area according to the time horizon data and logging data, including:

以时间层位数据为约束,利用反距离插值算法,对波阻抗曲线进行三维空间插值,确定波阻抗体。Constrained by the time horizon data, the wave impedance curve is interpolated in three dimensions by using the inverse distance interpolation algorithm to determine the wave impedance volume.

一个实施例中,一次波反射率转换模块按如下方式,将波阻抗体转换为一次波反射率:In one embodiment, the primary wave reflectivity conversion module converts the wave impedance body into the primary wave reflectivity as follows:

Figure BDA0001978522100000101
Figure BDA0001978522100000101

其中,r为一次波反射率;PI为波阻抗体;i为反射率采样点序号。Among them, r is the reflectivity of the primary wave; PI is the wave impedance body; i is the serial number of the reflectivity sampling point.

一个实施例中,所述数据获取模块获取的测井数据包括地震子波;In one embodiment, the logging data acquired by the data acquisition module includes seismic wavelets;

正演合成模块根据一次波反射率和测井数据,正演合成一次波地震记录,包括:The forward modeling synthesis module performs forward modeling and synthesis of primary wave seismic records according to the primary wave reflectivity and logging data, including:

将一次波反射率和地震子波进行褶积计算,正演合成一次波地震记录。The primary wave reflectivity and seismic wavelet are convolved and calculated, and the primary wave seismic records are synthesized by forward modeling.

一个实施例中,所述数据获取模块获取的测井数据包括地震子波;In one embodiment, the logging data acquired by the data acquisition module includes seismic wavelets;

正演合成模块根据一次波反射率和测井数据,正演合成全波地震记录,包括:The forward synthesis module performs forward synthesis of full-wave seismic records based on primary wave reflectivity and logging data, including:

根据一次波反射率,确定全波反射率;Determine the total wave reflectivity according to the primary wave reflectivity;

将全波反射率和地震子波进行褶积计算,正演合成全波地震记录。The full-wave reflectivity and seismic wavelet are convolved and calculated, and the full-wave seismic records are synthesized by forward modeling.

一个实施例中,多次波干扰区域确定模块根据一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域,包括:In one embodiment, the multiple wave interference area determination module determines multiple wave interference areas of different interference levels from the seismic work area according to the primary wave seismic records and the full wave seismic records, including:

根据一次波地震记录和全波地震记录,确定多次波地震记录;According to the primary wave seismic record and the full wave seismic record, determine the multiple wave seismic record;

根据一次波地震记录和多次波地震记录,确定信噪比属性切片;Determine the SNR attribute slice based on primary seismic records and multiple seismic records;

根据信噪比属性切片,从地震工区中确定不同干扰等级的多次波干扰区域。According to the SNR attribute slice, multiple wave interference areas with different interference levels are determined from the seismic work area.

一个实施例中,多次波干扰区域确定模块根据一次波地震记录和全波地震记录,确定多次波地震记录,包括:In one embodiment, the multiple wave interference area determination module determines the multiple wave seismic records according to the primary wave seismic records and the full wave seismic records, including:

将全波地震记录减去一次波地震记录,得到多次波地震记录。The primary seismic record is subtracted from the full seismic record to obtain the multiple seismic record.

一个实施例中,多次波干扰区域确定模块根据一次波地震记录和多次波地震记录,确定信噪比属性切片,包括:In one embodiment, the multiple wave interference area determination module determines the SNR attribute slice according to the primary wave seismic record and the multiple wave seismic record, including:

对一次波地震记录沿时间层位提取属性值,获得一次波沿层属性切片;Extract the attribute value along the time horizon from the primary wave seismic record, and obtain the primary wave along the layer attribute slice;

对多次波地震记录沿时间层位提取属性值,获得多次波沿层属性切片;Extract attribute values along the time horizon for multiple seismic records, and obtain attribute slices of multiple waves along the layer;

根据一次波沿层属性切片和多次波沿层属性切片,确定信噪比属性切片。The SNR attribute slice is determined according to the primary wave along-layer attribute slice and the multiple wave along-layer attribute slice.

一个实施例中,多次波干扰区域确定模块根据一次波沿层属性切片和多次波沿层属性切片,确定信噪比属性切片,包括:In one embodiment, the multiple wave interference area determination module determines the SNR attribute slice according to the primary wave along the layer attribute slice and the multiple wave along the layer attribute slice, including:

将一次波沿层属性切片与多次波沿层属性切片的比值确定为信噪比属性切片。The ratio of the primary wave along the layer attribute slice to the multiple wave along the layer attribute slice is determined as the signal-to-noise ratio attribute slice.

一个实施例中,多次波干扰区域确定模块根据信噪比属性切片,从地震工区中确定不同干扰等级的多次波干扰区域,包括:In one embodiment, the multiple wave interference area determination module determines multiple wave interference areas of different interference levels from the seismic work area according to the signal-to-noise ratio attribute slice, including:

将信噪比属性切片的值大于2的多次波干扰区域,确定为地震工区中第一干扰等级的多次波干扰区域;The multiple wave interference area where the value of the SNR attribute slice is greater than 2 is determined as the multiple wave interference area of the first interference level in the seismic work area;

将信噪比属性切片的值大于1小于2的多次波干扰区域,确定为地震工区中第二干扰等级的多次波干扰区域;The multiple wave interference area with the value of the signal-to-noise ratio attribute slice greater than 1 and less than 2 is determined as the multiple wave interference area of the second interference level in the seismic work area;

将信噪比属性切片的值小于1的多次波干扰区域,确定为地震工区中第三干扰等级的多次波干扰区域;The multiple wave interference area where the value of the SNR attribute slice is less than 1 is determined as the third interference level multiple wave interference area in the seismic work area;

其中,第一干扰等级小于第二干扰等级,第二干扰等级小于第三干扰等级。Wherein, the first interference level is smaller than the second interference level, and the second interference level is smaller than the third interference level.

综上,本发明实施例提供的一种识别多次波的方法和装置,通过建立波阻抗体,利用反射率正演模拟方法正演合成一次波地震记录和全波地震记录;通过对全波地震记录和一次波地震记录分析,得到多次波在某个地质层在平面上的能量分布,相对现有技术中多次波单点、单线的识别方法,本发明实施例能够对整个地震工区多次波的整体发育程度和分布情况进行预测,用于分析潜在多次波特征,应用在多次波压制处理中,从而实现多次波压制处理参数优选,一定程度上减少了压制多次波的不确定性;本发明实施例还能够根据划分的不同干扰等级多次波干扰区域,评价地震资料品质,划分出地震资料不可靠的区域,从而减小储层预测的多解性,降低井位部署的风险。本发明实施例仅需时间层位数据、测井数据和常规反演软件,无需地震处理软件和处理人员参与,实现过程简单,效率高。本发明实施例能够得到每个地质层的信噪比平面分布,直接应用于井位部署,实用性较强。To sum up, the embodiment of the present invention provides a method and device for identifying multiple waves. By establishing an acoustic impedance volume, the reflectivity forward modeling method is used to forward synthesize primary wave seismic records and full-wave seismic records; Seismic records and primary wave seismic records are analyzed to obtain the energy distribution of multiple waves in a certain geological layer on the plane. Compared with the identification method of multiple wave single point and single line in the prior art, the embodiment of the present invention can identify the entire seismic work area. The overall development degree and distribution of multiple waves are predicted, used to analyze potential multiple wave characteristics, and applied in multiple wave suppression processing, so as to realize the optimization of multiple wave suppression processing parameters and reduce the suppression of multiple waves to a certain extent. Uncertainty; the embodiment of the present invention can also evaluate the quality of seismic data according to the divided multiple interference areas of different interference levels, and divide the unreliable areas of seismic data, thereby reducing the ambiguity of reservoir prediction and reducing the number of wells. Bit deployment risk. The embodiment of the present invention only needs time horizon data, logging data and conventional inversion software, and does not need seismic processing software and processing personnel to participate, so the realization process is simple and efficient. The embodiment of the present invention can obtain the signal-to-noise ratio plane distribution of each geological layer, which can be directly applied to well location deployment, and has strong practicability.

本领域内的技术人员应明白,本发明的实施例可提供为方法、系统、或计算机程序产品。因此,本发明可采用完全硬件实施例、完全软件实施例、或结合软件和硬件方面的实施例的形式。而且,本发明可采用在一个或多个其中包含有计算机可用程序代码的计算机可用存储介质(包括但不限于磁盘存储器、CD-ROM、光学存储器等)上实施的计算机程序产品的形式。Those skilled in the art should understand that the embodiments of the present invention may be provided as methods, systems, or computer program products. Accordingly, the present invention can take the form of an entirely hardware embodiment, an entirely software embodiment, or an embodiment combining software and hardware aspects. Furthermore, the present invention may take the form of a computer program product embodied on one or more computer-usable storage media (including but not limited to disk storage, CD-ROM, optical storage, etc.) having computer-usable program code embodied therein.

本发明是参照根据本发明实施例的方法、设备(系统)、和计算机程序产品的流程图和/或方框图来描述的。应理解可由计算机程序指令实现流程图和/或方框图中的每一流程和/或方框、以及流程图和/或方框图中的流程和/或方框的结合。可提供这些计算机程序指令到通用计算机、专用计算机、嵌入式处理机或其他可编程数据处理设备的处理器以产生一个机器,使得通过计算机或其他可编程数据处理设备的处理器执行的指令产生用于实现在流程图一个流程或多个流程和/或方框图一个方框或多个方框中指定的功能的装置。The present invention is described with reference to flowchart illustrations and/or block diagrams of methods, apparatus (systems), and computer program products according to embodiments of the invention. It should be understood that each procedure and/or block in the flowchart and/or block diagram, and a combination of procedures and/or blocks in the flowchart and/or block diagram can be realized by computer program instructions. These computer program instructions may be provided to a general purpose computer, special purpose computer, embedded processor, or processor of other programmable data processing equipment to produce a machine such that the instructions executed by the processor of the computer or other programmable data processing equipment produce a An apparatus for realizing the functions specified in one or more procedures of the flowchart and/or one or more blocks of the block diagram.

这些计算机程序指令也可存储在能引导计算机或其他可编程数据处理设备以特定方式工作的计算机可读存储器中,使得存储在该计算机可读存储器中的指令产生包括指令装置的制造品,该指令装置实现在流程图一个流程或多个流程和/或方框图一个方框或多个方框中指定的功能。These computer program instructions may also be stored in a computer-readable memory capable of directing a computer or other programmable data processing apparatus to operate in a specific manner, such that the instructions stored in the computer-readable memory produce an article of manufacture comprising instruction means, the instructions The device realizes the function specified in one or more procedures of the flowchart and/or one or more blocks of the block diagram.

这些计算机程序指令也可装载到计算机或其他可编程数据处理设备上,使得在计算机或其他可编程设备上执行一系列操作步骤以产生计算机实现的处理,从而在计算机或其他可编程设备上执行的指令提供用于实现在流程图一个流程或多个流程和/或方框图一个方框或多个方框中指定的功能的步骤。These computer program instructions can also be loaded onto a computer or other programmable data processing device, causing a series of operational steps to be performed on the computer or other programmable device to produce a computer-implemented process, thereby The instructions provide steps for implementing the functions specified in the flow chart or blocks of the flowchart and/or the block or blocks of the block diagrams.

以上所述的具体实施例,对本发明的目的、技术方案和有益效果进行了进一步详细说明,所应理解的是,以上所述仅为本发明的具体实施例而已,并不用于限定本发明的保护范围,凡在本发明的精神和原则之内,所做的任何修改、等同替换、改进等,均应包含在本发明的保护范围之内。The specific embodiments described above have further described the purpose, technical solutions and beneficial effects of the present invention in detail. It should be understood that the above descriptions are only specific embodiments of the present invention and are not intended to limit the scope of the present invention. Protection scope, within the spirit and principles of the present invention, any modification, equivalent replacement, improvement, etc., shall be included in the protection scope of the present invention.

Claims (20)

1.一种识别多次波的方法,其特征在于,包括:1. A method for identifying multiple waves, comprising: 获取地震工区的时间层位数据和测井数据;Obtain the time horizon data and logging data of the seismic work area; 根据时间层位数据和测井数据,确定地震工区的波阻抗体;Determine the wave impedance volume of the seismic work area according to the time horizon data and logging data; 将波阻抗体转换为一次波反射率;Convert wave impedance volume to primary wave reflectivity; 根据一次波反射率和测井数据,正演合成一次波地震记录和全波地震记录;Based on the primary wave reflectivity and logging data, forward synthetic primary wave seismic records and full wave seismic records; 根据一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域;According to primary wave seismic records and full wave seismic records, multiple wave interference areas with different interference levels are determined from the seismic work area; 其中,根据一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域,包括:Among them, according to primary wave seismic records and full wave seismic records, multiple wave interference areas with different interference levels are determined from the seismic work area, including: 根据一次波地震记录和全波地震记录,确定多次波地震记录;According to the primary wave seismic record and the full wave seismic record, determine the multiple wave seismic record; 根据一次波地震记录和多次波地震记录,确定信噪比属性切片;Determine the SNR attribute slice based on primary seismic records and multiple seismic records; 根据信噪比属性切片,从地震工区中确定不同干扰等级的多次波干扰区域。According to the SNR attribute slice, multiple wave interference areas with different interference levels are determined from the seismic work area. 2.如权利要求1所述的方法,其特征在于,所述测井数据包括波阻抗曲线;2. The method of claim 1, wherein the well logging data comprises a wave impedance curve; 根据时间层位数据和测井数据,确定地震工区的波阻抗体,包括:According to the time horizon data and logging data, determine the wave impedance volume of the seismic work area, including: 以时间层位数据为约束,利用反距离插值算法,对波阻抗曲线进行三维空间插值,确定波阻抗体。Constrained by the time horizon data, the wave impedance curve is interpolated in three dimensions by using the inverse distance interpolation algorithm to determine the wave impedance volume. 3.如权利要求1所述的方法,其特征在于,按如下方式,将波阻抗体转换为一次波反射率:3. The method according to claim 1, characterized in that, the wave impedance body is converted into primary wave reflectivity as follows:
Figure FDA0003914909490000011
Figure FDA0003914909490000011
其中,r为一次波反射率;PI为波阻抗体;i为反射率采样点序号。Among them, r is the reflectivity of the primary wave; PI is the wave impedance body; i is the serial number of the reflectivity sampling point.
4.如权利要求1所述的方法,其特征在于,所述测井数据包括地震子波;4. The method of claim 1, wherein the well logging data comprises seismic wavelets; 根据一次波反射率和测井数据,正演合成一次波地震记录,包括:Based on primary reflectivity and logging data, forward synthetic primary seismic records include: 将一次波反射率和地震子波进行褶积计算,正演合成一次波地震记录。The primary wave reflectivity and seismic wavelet are convolved and calculated, and the primary wave seismic records are synthesized by forward modeling. 5.如权利要求1所述的方法,其特征在于,所述测井数据包括地震子波;5. The method of claim 1, wherein the well logging data comprises seismic wavelets; 根据一次波反射率和测井数据,正演合成全波地震记录,包括:Based on the primary wave reflectivity and logging data, forward synthetic full-wave seismic records, including: 根据一次波反射率,确定全波反射率;Determine the total wave reflectivity according to the primary wave reflectivity; 将全波反射率和地震子波进行褶积计算,正演合成全波地震记录。The full-wave reflectivity and seismic wavelet are convolved and calculated, and the full-wave seismic records are synthesized by forward modeling. 6.如权利要求1所述的方法,其特征在于,根据一次波地震记录和全波地震记录,确定多次波地震记录,包括:6. The method according to claim 1, wherein, according to the primary seismic record and the full seismic record, determining the multiple seismic record comprises: 将全波地震记录减去一次波地震记录,得到多次波地震记录。The primary seismic record is subtracted from the full seismic record to obtain the multiple seismic record. 7.如权利要求1所述的方法,其特征在于,根据一次波地震记录和多次波地震记录,确定信噪比属性切片,包括:7. The method according to claim 1, wherein, according to the primary wave seismic record and the multiple wave seismic record, determining the SNR attribute slice comprises: 对一次波地震记录沿时间层位提取属性值,获得一次波沿层属性切片;Extract the attribute value along the time horizon from the primary wave seismic record, and obtain the primary wave along the layer attribute slice; 对多次波地震记录沿时间层位提取属性值,获得多次波沿层属性切片;Extract attribute values along the time horizon for multiple seismic records, and obtain attribute slices of multiple waves along the layer; 根据一次波沿层属性切片和多次波沿层属性切片,确定信噪比属性切片。The SNR attribute slice is determined according to the primary wave along-layer attribute slice and the multiple wave along-layer attribute slice. 8.如权利要求7所述的方法,其特征在于,根据一次波沿层属性切片和多次波沿层属性切片,确定信噪比属性切片,包括:8. The method according to claim 7, wherein, according to the primary wave along the layer attribute slice and the multiple wave along the layer attribute slice, determine the signal-to-noise ratio attribute slice, comprising: 将一次波沿层属性切片与多次波沿层属性切片的比值确定为信噪比属性切片。The ratio of the primary wave along the layer attribute slice to the multiple wave along the layer attribute slice is determined as the signal-to-noise ratio attribute slice. 9.如权利要求1所述的方法,其特征在于,根据信噪比属性切片,从地震工区中确定不同干扰等级的多次波干扰区域,包括:9. The method according to claim 1, characterized in that, according to the SNR attribute slice, the multiple wave interference area of different interference levels is determined from the seismic work area, including: 将信噪比属性切片的值大于2的多次波干扰区域,确定为地震工区中第一干扰等级的多次波干扰区域;The multiple wave interference area where the value of the SNR attribute slice is greater than 2 is determined as the multiple wave interference area of the first interference level in the seismic work area; 将信噪比属性切片的值大于1小于2的多次波干扰区域,确定为地震工区中第二干扰等级的多次波干扰区域;The multiple wave interference area with the value of the signal-to-noise ratio attribute slice greater than 1 and less than 2 is determined as the multiple wave interference area of the second interference level in the seismic work area; 将信噪比属性切片的值小于1的多次波干扰区域,确定为地震工区中第三干扰等级的多次波干扰区域;The multiple wave interference area where the value of the SNR attribute slice is less than 1 is determined as the third interference level multiple wave interference area in the seismic work area; 其中,第一干扰等级小于第二干扰等级,第二干扰等级小于第三干扰等级。Wherein, the first interference level is smaller than the second interference level, and the second interference level is smaller than the third interference level. 10.一种识别多次波的装置,包括:10. A device for identifying multiple waves, comprising: 数据获取模块,用于获取地震工区的时间层位数据和测井数据;The data acquisition module is used to acquire the time horizon data and logging data of the seismic work area; 波阻抗体确定模块,用于根据时间层位数据和测井数据,确定地震工区的波阻抗体;The acoustic impedance volume determination module is used to determine the acoustic impedance volume of the seismic work area according to the time horizon data and well logging data; 一次波反射率转换模块,用于将波阻抗体转换为一次波反射率;The primary wave reflectivity conversion module is used to convert the wave impedance body into the primary wave reflectivity; 正演合成模块,用于根据一次波反射率和测井数据,正演合成一次波地震记录和全波地震记录;The forward modeling synthesis module is used for forward modeling and synthesizing primary wave seismic records and full wave seismic records according to the primary wave reflectivity and logging data; 多次波干扰区域确定模块,用于根据一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域;The multiple wave interference area determination module is used to determine multiple wave interference areas of different interference levels from the seismic work area according to the primary wave seismic records and the full wave seismic records; 其中,多次波干扰区域确定模块根据一次波地震记录和全波地震记录,从地震工区中确定不同干扰等级的多次波干扰区域,包括:Among them, the multiple wave interference area determination module determines the multiple wave interference areas of different interference levels from the seismic work area according to the primary wave seismic records and the full wave seismic records, including: 根据一次波地震记录和全波地震记录,确定多次波地震记录;According to the primary wave seismic record and the full wave seismic record, determine the multiple wave seismic record; 根据一次波地震记录和多次波地震记录,确定信噪比属性切片;Determine the SNR attribute slice based on primary seismic records and multiple seismic records; 根据信噪比属性切片,从地震工区中确定不同干扰等级的多次波干扰区域。According to the SNR attribute slice, multiple wave interference areas with different interference levels are determined from the seismic work area. 11.如权利要求10所述的装置,其特征在于,所述数据获取模块获取的测井数据包括波阻抗曲线;11. The device according to claim 10, characterized in that, the logging data obtained by the data acquisition module comprises wave impedance curves; 波阻抗体确定模块根据时间层位数据和测井数据,确定地震工区的波阻抗体,包括:The acoustic impedance volume determination module determines the acoustic impedance volume of the seismic work area according to the time horizon data and logging data, including: 以时间层位数据为约束,利用反距离插值算法,对波阻抗曲线进行三维空间插值,确定波阻抗体。Constrained by the time horizon data, the wave impedance curve is interpolated in three dimensions by using the inverse distance interpolation algorithm to determine the wave impedance volume. 12.如权利要求10所述的装置,其特征在于,一次波反射率转换模块按如下方式,将波阻抗体转换为一次波反射率:12. The device according to claim 10, wherein the primary wave reflectivity conversion module converts the wave impedance body into primary wave reflectivity as follows:
Figure FDA0003914909490000031
Figure FDA0003914909490000031
其中,r为一次波反射率;PI为波阻抗体;i为反射率采样点序号。Among them, r is the reflectivity of the primary wave; PI is the wave impedance body; i is the serial number of the reflectivity sampling point.
13.如权利要求10所述的装置,其特征在于,所述数据获取模块获取的测井数据包括地震子波;13. The device according to claim 10, wherein the logging data obtained by the data acquisition module comprises seismic wavelets; 正演合成模块根据一次波反射率和测井数据,正演合成一次波地震记录,包括:The forward modeling synthesis module performs forward modeling and synthesis of primary wave seismic records according to the primary wave reflectivity and logging data, including: 将一次波反射率和地震子波进行褶积计算,正演合成一次波地震记录。The primary wave reflectivity and seismic wavelet are convolved and calculated, and the primary wave seismic records are synthesized by forward modeling. 14.如权利要求10所述的装置,其特征在于,所述数据获取模块获取的测井数据包括地震子波;14. The device according to claim 10, wherein the logging data obtained by the data acquisition module comprises seismic wavelets; 正演合成模块根据一次波反射率和测井数据,正演合成全波地震记录,包括:The forward synthesis module performs forward synthesis of full-wave seismic records based on primary wave reflectivity and logging data, including: 根据一次波反射率,确定全波反射率;Determine the total wave reflectivity according to the primary wave reflectivity; 将全波反射率和地震子波进行褶积计算,正演合成全波地震记录。The full-wave reflectivity and seismic wavelet are convolved and calculated, and the full-wave seismic records are synthesized by forward modeling. 15.如权利要求10所述的装置,其特征在于,多次波干扰区域确定模块根据一次波地震记录和全波地震记录,确定多次波地震记录,包括:15. The device according to claim 10, wherein the multiple wave interference area determination module determines the multiple wave seismic records according to the primary wave seismic records and the full wave seismic records, including: 将全波地震记录减去一次波地震记录,得到多次波地震记录。The primary seismic record is subtracted from the full seismic record to obtain the multiple seismic record. 16.如权利要求10所述的装置,其特征在于,多次波干扰区域确定模块根据一次波地震记录和多次波地震记录,确定信噪比属性切片,包括:16. The device according to claim 10, wherein the multiple wave interference area determination module determines the SNR attribute slice according to the primary wave seismic record and the multiple wave seismic record, comprising: 对一次波地震记录沿时间层位提取属性值,获得一次波沿层属性切片;Extract the attribute value along the time horizon from the primary wave seismic record, and obtain the primary wave along the layer attribute slice; 对多次波地震记录沿时间层位提取属性值,获得多次波沿层属性切片;Extract attribute values along the time horizon for multiple seismic records, and obtain attribute slices of multiple waves along the layer; 根据一次波沿层属性切片和多次波沿层属性切片,确定信噪比属性切片。The SNR attribute slice is determined according to the primary wave along-layer attribute slice and the multiple wave along-layer attribute slice. 17.如权利要求16所述的装置,其特征在于,多次波干扰区域确定模块根据一次波沿层属性切片和多次波沿层属性切片,确定信噪比属性切片,包括:17. The device according to claim 16, wherein the multiple wave interference area determination module determines the SNR attribute slice according to the primary wave along the layer attribute slice and the multiple wave along the layer attribute slice, comprising: 将一次波沿层属性切片和多次波沿层属性切片的比值确定为信噪比属性切片。The ratio of the primary wave along the layer attribute slice and the multiple wave along the layer attribute slice is determined as the signal-to-noise ratio attribute slice. 18.如权利要求10所述的装置,其特征在于,多次波干扰区域确定模块根据信噪比属性切片,从地震工区中确定不同干扰等级的多次波干扰区域,包括:18. The device according to claim 10, wherein the multiple wave interference area determination module determines the multiple wave interference area of different interference levels from the seismic work area according to the signal-to-noise ratio attribute slice, including: 将信噪比属性切片的值大于2的多次波干扰区域,确定为地震工区中第一干扰等级的多次波干扰区域;The multiple wave interference area where the value of the SNR attribute slice is greater than 2 is determined as the multiple wave interference area of the first interference level in the seismic work area; 将信噪比属性切片的值大于1小于2的多次波干扰区域,确定为地震工区中第二干扰等级的多次波干扰区域;The multiple wave interference area with the value of the signal-to-noise ratio attribute slice greater than 1 and less than 2 is determined as the multiple wave interference area of the second interference level in the seismic work area; 将信噪比属性切片的值小于1的多次波干扰区域,确定为地震工区中第三干扰等级的多次波干扰区域;The multiple wave interference area where the value of the SNR attribute slice is less than 1 is determined as the third interference level multiple wave interference area in the seismic work area; 其中,第一干扰等级小于第二干扰等级,第二干扰等级小于第三干扰等级。Wherein, the first interference level is smaller than the second interference level, and the second interference level is smaller than the third interference level. 19.一种计算机设备,包括存储器、处理器及存储在存储器上并可在处理器上运行的计算机程序,所述处理器执行所述计算机程序时实现权利要求1至9任一项所述识别多次波的方法。19. A computer device, comprising a memory, a processor, and a computer program stored on the memory and operable on the processor, when the processor executes the computer program, the recognition described in any one of claims 1 to 9 is realized multiple wave method. 20.一种计算机可读存储介质,所述计算机可读存储介质存储有执行实现权利要求1至9任一项所述识别多次波的方法的计算机程序。20. A computer-readable storage medium storing a computer program for implementing the method for identifying multiple waves according to any one of claims 1 to 9.
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