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SEG Technical Program Expanded Abstracts 2018最新文献

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Microseismic activity after 2+ years of CO2 injection at Quest Quest注入二氧化碳2年后的微地震活动
Pub Date : 2018-08-27 DOI: 10.1190/SEGAM2018-2996295.1
V. Bacci, Jeff Tan, A. Halladay, S. O’Brien
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引用次数: 1
Overcoming cycle skipping in full-waveform inversion by reducing the adjoint sources oscillations 通过减小伴随源振荡克服全波形反演中的周期跳变
Pub Date : 2018-08-27 DOI: 10.1190/SEGAM2018-2997681.1
P. Yong, Jianping Huang, Zhenchuan Li, Wenyuan Liao
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引用次数: 0
Application of instantaneous dominant-frequency attributes and gamma-ray wireline logs in the delineation of lithology in Serbin Field, Southeast Texas: A case study 瞬时主频率属性和伽马电缆测井在德克萨斯州东南部Serbin油田岩性圈定中的应用:一个案例研究
Pub Date : 2018-08-27 DOI: 10.1190/SEGAM2018-2983521.1
O. Ogiesoba, W. Ambrose, R. Loucks
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引用次数: 1
Effects of wrong adjoints for RTM in TTI media TTI介质中错误伴随对RTM的影响
Pub Date : 2018-08-27 DOI: 10.1190/SEGAM2018-2996274.1
M. Louboutin, Philipp A. Witte, F. Herrmann
In order to obtain accurate images of the subsurface, anisotropic modeling and imaging is necessary. However, the twenty-one parameter complete wave-equation is too computationally expensive to be of use in this case. The transverse tilted isotropic wave-equation is then the next best feasible representation of the physics to use for imaging. The main complexity arising from transverse tilted isotropic imaging is to model the receiver wavefield (back propagation of the data or data residual) for the imaging condition. Unlike the isotropic or the full physics wave-equations, the transverse tilted isotropic wave-equation is not not self-adjoint. This difference means that time-reversal will not model the correct receiver wavefield and this can lead to incorrect subsurface images. In this work, we derive and implement the adjoint wave-equation to demonstrate the necessity of exact adjoint modeling for anisotropic modeling and compare our result with adjoint-free time-reversed imaging.
为了获得准确的地下图像,需要进行各向异性建模和成像。但是,21参数完全波动方程的计算成本太高,不能用于这种情况。横向倾斜的各向同性波动方程是下一个最好的可行的物理表征,用于成像。横向倾斜各向同性成像的主要复杂性是成像条件下的接收波场(数据的反向传播或数据残差)的建模。与各向同性或全物理波方程不同,横向倾斜各向同性波方程不是不自伴随的。这种差异意味着时间反转不能模拟正确的接收器波场,这可能导致不正确的地下图像。在这项工作中,我们推导并实现了伴随波方程,以证明在各向异性建模中精确伴随建模的必要性,并将我们的结果与伴随自由逆时成像进行了比较。
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引用次数: 7
Multiattribute reservoir parameter estimation based on a machine learning technique 基于机器学习技术的多属性油藏参数估计
Pub Date : 2018-08-27 DOI: 10.1190/SEGAM2018-2992296.1
Zhenyu Yuan, Handong Huang, Jiang Yuxin, Tang Jinbiao
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引用次数: 2
Study of intrinsic versus scattering attenuation of seismic waves from borehole measurements 钻孔测量地震波的本征衰减与散射衰减研究
Pub Date : 2018-08-27 DOI: 10.1190/SEGAM2018-2997036.1
A. Pirogova, B. Gurevich, R. Pevzner, S. Vlasov
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引用次数: 2
Signal analysis and time-frequency representation using SSA and adaptive AR methods 使用SSA和自适应AR方法的信号分析和时频表示
Pub Date : 2018-08-27 DOI: 10.1190/SEGAM2018-2995661.1
M. Porsani, B. Ursin, Michelângelo G. Silva
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引用次数: 3
Constraining the T2*-T2 relationship in surface nuclear magnetic resonance free-induction decay data 表面核磁共振自由感应衰变数据中T2*-T2关系的约束
Pub Date : 2018-08-27 DOI: 10.1190/SEGAM2018-2998133.1
D. Grombacher, G. Fiandaca, E. Auken
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引用次数: 0
Improved upscaling of steel-cased wells through inversion 通过反演提高了钢套井的增产效果
Pub Date : 2018-08-27 DOI: 10.1190/SEGAM2018-2998601.1
C. Schwarzbach, E. Haber
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引用次数: 6
Microseismic interpretation: From dots to the bigger picture 微地震解释:从点到大局
Pub Date : 2018-08-27 DOI: 10.1190/SEGAM2018-2998564.1
E. Ardakani, A. Baig
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引用次数: 1
期刊
SEG Technical Program Expanded Abstracts 2018
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