4.5 Article

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

Journal

TECTONOPHYSICS
Volume 712, Issue -, Pages 663-683

Publisher

ELSEVIER
DOI: 10.1016/j.tecto.2017.06.030

Keywords

Geomechanical modeling; In-situ stress field; Shale reservoir; Numerical simulation; Lower Cambrian; Cen'gong block

Funding

  1. National Natural Science Foundation of China [41372139, 41072098]
  2. National Science and Technology Major Project of China [2016ZX05046-003-001, 2016ZX05034-004-003]

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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.

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