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80th EAGE Conference and Exhibition 2018最新文献

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New Generation of Operational Absolute Gravimeter for Reservoir Monitoring 用于水库监测的新一代可操作绝对重力仪
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801465
J. Lautier Gaud, P. Vermeulen, N. Lemoigne, V. Ménoret, S. Bonvalot, B. Desruelle
Summary Reservoir monitoring, reservoir engineering, 4D gravity, time-lapse gravimetry, gravity survey, absolute gravimetry, subsidence monitoring, geothermal energy, carbon sequestration, enhanced oil recovery.
油藏监测、油藏工程、4D重力、延时重力、重力测量、绝对重力、沉降监测、地热能、固碳、提高采收率。
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引用次数: 0
Eigenray Tracing in 3D Heterogeneous Media 三维非均匀介质中的特征射线追踪
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801325
Z. Koren, I. Ravve
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引用次数: 1
Three-Dimensional Inversion and Interpretation of Multimodal Geophysical Data in Yamagawa Geothermal Field, Japan 日本山川地热田多模态地球物理资料三维反演与解释
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801186
M. Endo, M. Zhdanov, A. Gribenko, D. Sunwall, Takuya Miura, Hisako Mochinaga, N. Aoki, T. Mouri
Summary Exploration and development of geothermal fields requires quantitative interpretation of different geophysical data. In this paper, we introduce the novel approach to three-dimensional inversion and interpretation of multimodal geophysical data, which incorporates the known geological/geophysical constraints. In a general case, geophysical inverse problem is ill-posed, i.e., it is non-unique and unstable; however, appropriate a priori information can help reducing the nonuniqueness and increasing the stability of this ill-posed problem. The developed approach uses the principles of inversion “guided” by known information. In the framework of this approach, the 3D inversion itself is data driven, but a priori geological/geophysical model is used as the initial and reference model during the iterative inversion process. We have applied the developed method to the integrated interpretation of magnetotelluric, gravity, and magnetic data in Yamagawa geothermal field of Japan, using the constraints based on seismic and well-logging data acquired in the same area. The results have demonstrated that the developed method produces reliable 3D models of different physical properties, which provide a solid basis for geological interpretation of the complex subsurface structures in the survey area, critical for geothermal exploration.
地热田的勘探和开发需要对不同的地球物理资料进行定量解释。本文介绍了多模态地球物理数据三维反演和解释的新方法,该方法结合了已知的地质/地球物理约束条件。一般情况下,地球物理逆问题是不适定的,即它是非唯一的和不稳定的;然而,适当的先验信息可以帮助减少非唯一性,提高该病态问题的稳定性。开发的方法使用由已知信息“引导”的反演原理。在该方法的框架中,三维反演本身是数据驱动的,但在迭代反演过程中使用先验的地质/地球物理模型作为初始和参考模型。本文将该方法应用于日本山川地热田的大地电磁、重磁资料综合解释,利用同一地区地震和测井资料的约束条件。结果表明,该方法可生成可靠的不同物性的三维模型,为研究区复杂地下构造的地质解释提供了坚实的基础,对地热勘探具有重要意义。
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引用次数: 1
Source Type Classification Based On the Support Vector Machine Method 基于支持向量机方法的源类型分类
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801577
C. Song, T. Alkhalifah, Z. Wu
Summary Attaining information of the source mechanism involved in micro-seismic events will greatly help us understand the reservoir fracturing and the stress evolved. The components of moment tensor can tell us the information involving magnitudes, modes, and orientations of fractures. Meanwhile, its singular value decomposition (SVD) exposes the difference between three main kinds of source types that may present itself in a moment tensor solution. We propose to use support vector machine (SVM), which is a type of machine learning approach, to classify the source type of a micro-seismic event by using the normalized eigenvalues of moment tensor matrix as classification principal components. The tests on moment tensor matrices based on typical source type and real cases yield reliable classification results.
获取微震事件的震源机制信息,对了解储层压裂及应力演化具有重要意义。矩张量的分量可以告诉我们裂缝的大小、模式和方向等信息。同时,它的奇异值分解(SVD)揭示了在矩张量解中可能出现的三种主要源类型之间的差异。本文提出使用支持向量机(SVM)作为一种机器学习方法,利用矩张量矩阵的归一化特征值作为分类主成分,对微地震事件的源类型进行分类。基于典型源类型和实际案例的矩张量矩阵测试得到了可靠的分类结果。
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引用次数: 4
P-And S-Wave Separated Elastic Reverse Time Migration for OBS Data from Fluid-Solid Media with Irregular Seabed Interfac 不规则海底界面流固介质海底地震仪数据纵波和横波分离弹性逆时偏移
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201800979
Y. Qu, J. Li, Z. Li, J. Huang
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引用次数: 0
Subsalt 3-D Modelling and HC Reservoir Prediction with Scarce 2-D Seismic Datasets: Can We Obtain Reliable Results? 利用稀缺的二维地震资料进行盐下三维建模和HC储层预测:能否获得可靠的结果?
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801424
O. Petrovskyy, T. O. Fedchenko, N. S. Gangenko, V. Benko
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引用次数: 0
Geological Approach to the Optimization of Production Rates by Identifying Depositional Systems 通过识别沉积体系来优化产量的地质方法
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801256
B. Sorani
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引用次数: 0
An Outlook on Seismic Diffraction Imaging Using Pattern Recognition 模式识别在地震衍射成像中的应用展望
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201800634
B. Lowney, I. Lokmer, C. Bean, G. O'Brien, M. Igoe
A seismic image is formed by interactions of the seismic wavefield with geological interfaces, in the form of reflections, diffractions, and other coherent noise. While in conventional processing workflows reflections are favoured over diffractions, this is only beneficial in areas with uniform stratigraphy. Diffractions form as interactions of the wavefield with discontinuities and therefore can be used to image them. However, to image diffractions, they must first be separated from the seismic wavefield. Here we propose a pattern recognition approach for separation, employing image segmentation. We then compare this to two existing diffraction imaging methods, plane-wave destruction and f-k filtering. Image segmentation can be used to divide the image into pixels which share certain criteria. Here, we have separated the image first by amplitude using a histogram-based segmentation method, followed by edge detection with a Sobel operator to locate the hyperbola. The image segmentation method successfully locates diffraction hyperbola which can then be separated and migrated for diffraction imaging. When compared with plane-wave destruction and f-k filtering, the image segmentation method proves beneficial as it allows for identification of the hyperbolae without noise. However, the method can fail to identify hyperbolae in noisier environments and when hyperbolae overlap.
地震图像是由地震波场与地质界面以反射、衍射和其他相干噪声的形式相互作用形成的。虽然在传统的处理工作流程中,反射比衍射更有利,但这只在地层均匀的地区有益。衍射形成与不连续的波场的相互作用,因此可以用来成像。然而,为了成像衍射,它们必须首先从地震波场中分离出来。在这里,我们提出了一种模式识别方法的分离,采用图像分割。然后,我们将其与两种现有的衍射成像方法,平面波破坏和f-k滤波进行了比较。图像分割可用于将图像划分为共享某些标准的像素。在这里,我们首先使用基于直方图的分割方法通过幅度分离图像,然后使用Sobel算子进行边缘检测以定位双曲线。图像分割方法成功地定位了衍射双曲线,并对其进行了分离和迁移,实现了衍射成像。当与平面波破坏和f-k滤波相比较时,图像分割方法被证明是有益的,因为它允许在没有噪声的情况下识别双曲线。然而,该方法在噪声环境和双曲线重叠时无法识别双曲线。
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引用次数: 4
The Impact of Reservoir Heterogeneities on P-wave Propagation at Low Frequencies – Examples from the North Sea 储层非均质性对低频纵波传播的影响——以北海为例
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801453
E. Chabyshova, G. Goloshubin, S. Ahmad
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引用次数: 1
Development of a Predictive Model for Enhanced Gas Recovery by CO2 Huff-n-Puff in Depleted Carbonate Gas Reservoirs 枯竭碳酸盐岩气藏CO2吞吐提高采收率预测模型的建立
Pub Date : 2018-06-11 DOI: 10.3997/2214-4609.201801559
Edo Pratama, M. Ismail, S. Ridha
Injecting CO2 with huff-n-puff process is becoming an efficient technique to overcome some productivity damage and enhanced gas recovery in depleted gas reservoirs. Several numerical simulations are required to estimate the gas recovery factor obtained from CO2 huff-n-puff injection. However, numerical simulations are very expensive and time-consuming processes.
在枯竭气藏中,利用吞吐法注入二氧化碳已成为克服产能损害和提高采收率的有效技术。需要进行多次数值模拟来估计CO2吞吐注入获得的采收率。然而,数值模拟是非常昂贵和耗时的过程。
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引用次数: 0
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80th EAGE Conference and Exhibition 2018
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