A'/> 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
首页> 外文期刊>Tectonophysics: International Journal of Geotectonics and the Geology and Physics of the Interior of the Earth >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
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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

机译:页岩水库原位应力领域的3D地质力学建模与数值模拟 - 以南方岑松街区下寒武纪尼图恩形成的案例研究

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Abstract 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 (Δσ), horizontal stress difference coefficient (Kh), and stress type coefficient (Sp) 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 375m, the stress type is mainly a thrust faulting stress regime. At dep
机译:<![cdata [ 抽象 基于关于地下的综合信息进行页岩水库中的原位应力状态分析霍尔伯勒斯在开发石油和天然气场地建立的性质。工业水平的页岩气产量发生在南方下寒武纪岑松街区的Niutitang形成。在本研究中,已经采用了从液压压裂,钻孔诱导的骨折,钻孔突破,全球定位系统(GPS)和井偏差统计中获得的数据来确定最大水平主应力的取向。另外,使用液压压裂和多极阵列声测井(XMAC)来确定原位应力幅度的垂直变化。基于测井解释和机械实验,通过地震反转获得了机械参数的空间分布,并且使用有限元应力分析方法建立了3D异构地质力学模型来模拟原位应力场。深度,故障,岩石力学和层变化对主应力的影响,水平应力差(ΔΣ),水平应力差系数(K H ),和应力型系数(S P )。结果表明,最大主要应力的方向是ESE 120°。另外,自然骨折的开发区似乎与具有高主应力差异的区域相关。在深度浅375浅 m,应力型主要是推力断裂应力制度。在Dep.

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