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Reservoir Elastic Parameters Estimation from Surface Seismic Data Using JMI-res: A Full-Wavefield Approach 利用JMI-res从地面地震资料估计储层弹性参数:全波场方法
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201800726
A. Garg, S. Sharma, D. J. Verschuur
Summary Any target-oriented localised inversion scheme for reservoir elastic parameters is as good as the input dataset. Thus, the accuracy of the input dataset i.e. local reflection response or impulse response (virtual source-receiver response) is of utmost importance, especially when the target area is below a complex overburden. In these subsurface settings, the overburden internal multiples and associated transmission imprint obscure the local response, which in turn affects the estimated elastic parameters resolution. Here, we demonstrate a novel process called JMI-res, based on Joint Migration Inversion (JMI), to estimate the reservoir elastic parameters from the surface seismic elastic data for a complex subsurface scenario. In JMI-res, we first obtain the accurate local impulse responses at the target depth level, while correctly accounting for overburden internal multiples and then we apply a localized inversion scheme on the estimated impulse responses to get the reservoir elastic parameters. Moreover, the propagation velocity estimation is an integral part of JMI-res. In this paper, we show that JMI-res provides much more reliable local target impulse responses, thus yielding high-resolution elastic parameters, compared to standard redatuming based on time reversal of recorded data, courtesy of proper handling of internal multiples in the redatuming step.
任何面向目标的储层弹性参数局部反演方案都与输入数据集一样好。因此,输入数据集的准确性,即局部反射响应或脉冲响应(虚拟源-接收机响应)是至关重要的,特别是当目标区域位于复杂覆盖层下方时。在这些地下环境中,覆盖层内部倍数和相关的传输印记掩盖了局部响应,从而影响了估计的弹性参数分辨率。在这里,我们展示了一种新的方法,称为JMI-res,基于联合迁移反演(JMI),从复杂的地下场景的地面地震弹性数据中估计储层弹性参数。在JMI-res中,首先在正确考虑覆盖层内倍数的情况下,在目标深度得到准确的局部脉冲响应,然后对估计的脉冲响应应用局部反演方案,得到储层弹性参数。此外,传播速度估计是JMI-res的重要组成部分。在本文中,我们证明了JMI-res提供了更可靠的局部目标脉冲响应,从而产生高分辨率的弹性参数,与基于记录数据的时间反演的标准重数据相比,由于在重数据步骤中正确处理了内部倍数。
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引用次数: 7
Wavefield Transmission Imaging with Reverse Time Migration 具有逆时偏移的波场透射成像
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201800652
C. Willacy, M. Kryvohuz
Steep salt boundaries can be poorly illuminated or completely absent in the migrated image. To provide a solution to this problem, we apply two reverse time migration imaging methods which use transmitted (refracted) wavefields. In the first technique, down-going waves, typically recorded in walkaway VSP surveys, are used to image the salt flank via the generation of aplanatic isochrones. It is demonstrated that this image can be generated in the absence of an explicit interpretation of the salt flank. In the second technique, we extend the basic theory to include imaging of up-going source wave fields which then refract at the base salt, as acquired by a surface acquisition geometry. This technique has similarities to the prism-imaging method, yet it uses transmitted instead of reflected waves at the salt boundary. We demonstrate that this is not only a viable technique for imaging of the salt boundary, but also to determine the correct salt velocity when used in conjunction with conventional reflection imaging. A combination of synthetic and field datasets is used to demonstrate the transmission imaging methodologies for imaging salt flanks with reverse time migration.
在迁移图像中,陡峭的盐边界可能照明不佳或完全不存在。为了解决这一问题,我们采用了两种利用透射(折射)波场的逆时偏移成像方法。在第一种技术中,下行波(通常记录在走开式VSP测量中)通过生成无平面等时线来对盐侧进行成像。结果表明,该图像可以在没有明确解释盐翼的情况下生成。在第二种技术中,我们扩展了基本理论,包括上行源波场的成像,然后在基盐处折射,这是通过表面采集几何图形获得的。这种技术与棱镜成像方法有相似之处,但它在盐界使用透射波而不是反射波。我们证明,这不仅是一种可行的盐边界成像技术,而且当与常规反射成像结合使用时,也可以确定正确的盐速度。结合合成数据集和现场数据集,演示了对具有逆时偏移的盐侧翼进行成像的透射成像方法。
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引用次数: 0
Application of 3D seismic to Enhance Mapping of Potholes in the Western Bushveld Complex, South Africa 应用三维地震增强南非西部Bushveld复合体凹坑的测绘
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801715
L. Sehoole, M. Manzi, S. Zhang
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引用次数: 0
Anisotropic Wide Azimuth 3D Seismic Data for an Unconventional Shale Oil Project, Aguada Federal Block, Argentina 阿根廷Aguada联邦区块非常规页岩油项目的各向异性宽方位三维地震数据
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801063
D. Curia, P. Veeken, D. Justo, Martín Alayón
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引用次数: 1
Simulating the Influence of Micro-Pore Structure on Mud Invasion Using the Digital Rock Technology 利用数字岩石技术模拟微孔结构对泥浆侵入的影响
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201800962
X. Zeng, J. Sun, H. Dong, L. Cui
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引用次数: 0
Enhanced Resolution of Reflection GPR Data by Diffraction Imaging 利用衍射成像技术提高反射GPR数据的分辨率
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201800950
Hemin Yuan, M. Montazeri, M. Looms, J. Kammann, L. Nielsen
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引用次数: 0
Ground Roll Attenuation Applying Matching Pursuit Algorithm 应用匹配跟踪算法抑制地滚
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201800934
S. Chen, Y. Li, J. Cheng
Summary The main characteristics of ground roll are dispersion, low frequency, low velocity and high amplitude. It significantly affects the quality of the seismic data as a kind of noise and is necessary to be subtracted from the original data. Common ground roll attenuation methods include band-pass filtering, f-k filtering and so on, but the effective signal is inevitably harmed in the denoising process. In this paper, ground roll noise is extracted by using matching pursuit (MP) algorithm. Low frequency as the feature of ground roll can be identified as atom, and the time shift parameter is also employed to preserve the effective signal. Synthetic example shows that the ground roll is attenuated and the effective signal is preserved in the events that are polluted seriously by the ground roll noise. Application of field data proves the efficiency and superiority of matching pursuit algorithm compared with band-pass filtering and f-k filtering.
地滚的主要特点是频散、低频、低速、高幅值。它作为一种噪声,对地震资料的质量有很大的影响,必须从原始资料中去除。常用的地滚衰减方法有带通滤波、f-k滤波等,但在去噪过程中不可避免地会损害有效信号。本文采用匹配追踪(MP)算法提取地滚噪声。低频作为地滚的特征可以被识别为原子,并利用时移参数来保持有效信号。综合算例表明,在受地滚噪声严重污染的事件中,地滚信号得到了衰减,有效信号得以保留。现场数据的应用证明了匹配跟踪算法相对于带通滤波和f-k滤波的有效性和优越性。
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引用次数: 1
The Strong Effect of Compaction on Elastic Properties of Rocks, (An Example of a Poorly Consolidated Formation from Russ 压实作用对岩石弹性特性的强烈影响(以俄罗斯一种弱胶结地层为例)
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801081
L. Uspenskaya
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引用次数: 0
Forward Kirchhoff Modelling to Evaluate Potential Interpretation Pitfalls beneath Sub-vertical Velocity Discontinuities 正演Kirchhoff模型评估次垂直速度不连续下潜在的解释缺陷
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801446
L. Zühlsdorff, A. Atkinson, H. Gjøystdal, T. Kaschwich, A.J.S. Wilson
Summary Sharp velocity contrasts in the overburden may cause problems for seismic imaging of deeper targets. Pre-stack depth migration in combination with traveltime tomography to build the velocity model is generally considered as a solution to the problem. However, building the velocity model with sufficient lateral and vertical resolution near discontinuities is difficult and imperfect velocity models will result in imperfect seismic images. Forward modelling seismic data followed by PSDM is a way to investigate and quantify sensitivity to imperfections in the velocity model. Kirchhoff modelling offers an efficient alternative to full-wavefield modelling; it is based on advanced ray tracing and can model diffractions, but is still computationally quick. In this study Kirchhoff pre-stack modelling provides a means for testing the impact of velocity errors on the final seismic image: Kirchoff modelling is followed by Kirchhoff target migration with the model velocity field and with degraded velocity fields. Results reveal the scale of potential imaging errors under a shallow velocity discontinuity at the Golden Eagle field in the North Sea. Results show that the danger of creating false structure due to image distortion is low, but that vertical positioning due to inaccurate velocity models carries a higher risk.
上覆层中速度差较大可能会给深部目标的地震成像带来问题。叠前深度偏移结合走时层析成像建立速度模型通常被认为是解决这一问题的一种方法。然而,在不连续面附近建立具有足够水平和垂直分辨率的速度模型是困难的,并且速度模型不完善将导致地震图像不完善。利用PSDM对地震数据进行正演模拟是一种研究和量化速度模型中缺陷敏感性的方法。基尔霍夫建模提供了一个有效的替代全波场建模;它是基于先进的光线追踪,可以模拟衍射,但仍然是计算快。在本研究中,Kirchhoff叠前建模为测试速度误差对最终地震图像的影响提供了一种手段:Kirchhoff建模之后是Kirchhoff目标与模型速度场和退化速度场的偏移。结果揭示了北海金鹰油田浅层速度不连续下潜在成像误差的规模。结果表明,由于图像失真而产生虚假结构的风险较低,但由于速度模型不准确而导致的垂直定位风险较高。
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引用次数: 0
Low-Frequency Data Extrapolation Using a Feed-Forward ANN 基于前馈神经网络的低频数据外推
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801231
O. Ovcharenko, V. Kazei, D. Peter, X. Zhang, T. Alkhalifah
Full-waveform inversion (FWI) benefits in many ways from having low-frequency data. However, those are rarely available due to acquisition limitations. Here, we explore the feasibility of frequency-bandwidth extrapolation using an Artificial Neural Network (ANN) approach. The ANN is trained to be a non-linear operator that maps high-frequency data for a single source and multiple receivers to low-frequency data. Assuming that the source is a point (delta function) in both time and space, we train the network on synthetic data generated using random velocity models. Extending our previous work, we apply the ANN to multiple collocated source-receiver acquisitions to predict 0.5~Hz data for a crop from the acoustic BP 2004 benchmark model. Prediction results, in general, resemble the reference ones but the prediction accuracy is barely sufficient to directly use extrapolated data in FWI. To demonstrate, we show regularized mono-frequency FWI on extrapolated data.
全波形反演(FWI)在很多方面都得益于低频数据。然而,由于收购限制,这些设备很少可用。在这里,我们探讨了使用人工神经网络(ANN)方法进行频率-带宽外推的可行性。人工神经网络被训练成一个非线性算子,将单一来源和多个接收器的高频数据映射到低频数据。假设源在时间和空间上都是一个点(delta函数),我们使用随机速度模型生成的合成数据来训练网络。扩展我们之前的工作,我们将人工神经网络应用于多个并置的源接收机采集,以从声学BP 2004基准模型中预测作物的0.5~Hz数据。一般情况下,预测结果与参考结果相似,但预测精度不足以直接使用外推数据进行FWI预测。为了证明这一点,我们在外推数据上展示了正则化的单频FWI。
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引用次数: 31
期刊
80th EAGE Conference and Exhibition 2018
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