3D geomechanical modeling and numerical simulation of in-situ stress fields in shale reservoirs: A case study of the lower Cambrian Niutitang formation in the Cen'gong block, South China

被引:91
作者
Liu, Jingshou [1 ,2 ,3 ,4 ]
Ding, Wenlong [1 ,2 ,3 ,4 ]
Yang, Haimeng [5 ]
Wang, Ruyue [6 ,7 ]
Yin, Shuai [8 ]
Li, Ang [1 ]
Fu, Fuquan [1 ]
机构
[1] China Univ Geosci, Sch Energy Resources, Beijing 100083, Peoples R China
[2] China Univ Geosci, Minist Educ, Key Lab Marine Reservoir Evolut & Hydrocarbon Abu, Beijing 100083, Peoples R China
[3] China Univ Geosci, Beijing Key Lab Unconvent Nat Gas Geol Evaluat &, Beijing 100083, Peoples R China
[4] China Univ Geosci, Minist Land & Resources, Key Lab Shale Gas Exploitat & Assessment, Beijing 100083, Peoples R China
[5] SINOPEC, Zhongyuan Oilfield Co Ltd, Oil Recovery Plant 3, Puyang 066004, Henan, Peoples R China
[6] State Key Lab Shale Oil & Gas Enrichment Mech & E, Beijing 100083, Peoples R China
[7] SINOPEC, Petr Explorat & Prod Res Inst, Beijing 100083, Peoples R China
[8] Xian Shiyou Univ, Sch Earth Sci & Engn, Xian 710065, Shaanxi, Peoples R China
基金
中国国家自然科学基金;
关键词
Geomechanical modeling; In-situ stress field; Shale reservoir; Numerical simulation; Lower Cambrian; Cen'gong block; QUANTITATIVE PREDICTION; FRACTURE-ANALYSIS; REGIONAL STRESS; TECTONIC STRESS; CRUSTAL STRESS; BASIN; SEDIMENTARY; ORIENTATION; DEPRESSION; ZONES;
D O I
10.1016/j.tecto.2017.06.030
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
An analysis of the in-situ state of stress in a shale reservoir was performed based on comprehensive information about the subsurface properties from wellbores established during the development of an oil and gas field. Industrial-level shale gas production has occurred in the Niutitang formation of the lower Cambrian Cen'gong block, South China. In this study, data obtained -from hydraulic fracturing, drilling-induced fractures, borehole breakout, global positioning system (GPS), and well deviation statistics have been used to determine the orientation of the maximum horizontal principal stress. Additionally, hydraulic fracturing and multi-pole array acoustic logging (XMAC) were used to determine the vertical variations in the in-situ stress magnitude. Based on logging interpretation and mechanical experiments, the spatial distributions of mechanical parameters were obtained by seismic inversion, and a 3D heterogeneous geomechanical model was established using a finite element stress analysis approach to simulate the in-situ stress fields. The effects of depth, faults, rock mechanics, and layer variations on the principal stresses, horizontal stress difference (Delta sigma), horizontal stress difference coefficient (K-h), and stress type coefficient (S-p) were determined. The results show that the direction of the maximum principal stress is ESE 120. Additionally, the development zones of natural fractures appear to correlate with regions with high principal stress differences. At depths shallower than 375 m, the stress type is mainly a thrust faulting stress regime. At depths ranging from 375 to 950 m, the stress type is mainly a strike-slip faulting stress regime. When the depth is >950 m, the stress type is mainly a normal faulting stress regime. Depth, fault orientation, and rock mechanics all affect the type of stress. The knowledge regarding the Cen'gong block is reliable and can improve borehole stability, casing set point determination, well deployment optimization, and fracturing area selection. (C) 2017 Elsevier B.V. All rights reserved.
引用
收藏
页码:663 / 683
页数:21
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