Simulating a High-Resolution Tectonic Stress Field and Predicting the Fracture Distributions in Shale Reservoirs Based on a Heterogeneous Rock Mechanics Model with Adaptive Boundary Condition Constraints

被引:0
作者
Lu, Lin [1 ]
Liu, Jingshou [2 ]
Luo, Yang [2 ]
Lu, Yuanhong [3 ]
Zhang, Binxin [3 ]
Yang, Haimeng [4 ]
机构
[1] China Univ Geosci, Key Lab Tecton & Petr Resources, Minist Educ, Wuhan 430074, Peoples R China
[2] China Univ Geosci, Sch Earth Resources, Wuhan 430074, Peoples R China
[3] China Univ Geosci, Wuhan 430074, Peoples R China
[4] Shandong Univ Sci & Technol, Coll Earth Sci & Engn, Qingdao 266590, Peoples R China
基金
中国国家自然科学基金;
关键词
Shale reservoir; Tectonic stress field; Numerical simulation; Fractures; Lower Cambrian; IN-SITU STRESS; CAMBRIAN NIUTITANG FORMATION; CENGONG BLOCK; SANGZHI BLOCK; MARINE SHALE; DEVELOPMENTAL CHARACTERISTICS; NATURAL FRACTURES; ORGANIC-RICH; BASIN; EXAMPLE;
D O I
10.1061/IJGNAI.GMENG-9727
中图分类号
P5 [地质学];
学科分类号
0709 ; 081803 ;
摘要
Obtaining higher-resolution and more realistic characteristics of tectonic stress fields is the goal of research into tectonic stress field simulations. In this study, a regional heterogeneous rock mechanics model was established on the basis of seismic, logging, and sample experimental data. The simulation results show that the minimum principal stress values in the lower Niutitang formation are between 25.0 and 120.0 MPa. The quantitative distribution prediction results for shale reservoir fractures based on the high-resolution tectonic stress field numerical model show that the fracture development zones in the Sangzhi block are mainly distributed near the fault, fold axis turning, and fold wing in an NE-SW orientation. There are two types of fractures developed in this region: shear fractures and tensile fractures. The shear fractures mainly developed near the NE-SW-oriented faults, with shear fracture rates ranging from 1 to 3, and the tensile fractures mainly developed in the southeast wing of the Wudaoshui anticline, with tensile fracture rates ranging from 1 to 2. The low fracture development zone is mainly located in the western slope of the block, with shear fracture rates and tensile fracture rates that are both < 1. (c) 2024 American Society of Civil Engineers.
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页数:13
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