Lithology-controlled stress variations of Longmaxi shale – Example of an appraisal wellbore in the Changning area

Xiaodong Ma , Shihuai Zhang , Xiaowen Zhang , Jiandong Liu , Juan Jin , Wei Cheng , Weidong Jiang , Guangming Zhang , Zhaowei Chen , Mark D. Zoback
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引用次数: 12

Abstract

The Longmaxi shale is an extensive, prolific unconventional play in southwestern China. Its development in the Changning area is affected by ineffective hydraulic fracturing (HF) stimulation, fault reactivation and casing damage. It is suspected that the stress contrast within and between the shale reservoirs and the formations above and below matters to hydraulic fracture propagation and reservoir stimulation. To this end, the Longmaxi shale in the Changning area deserves a dedicated quantification of the in situ stress state and its variations. In this study, we re-visit the available data from one of the play’s first appraisal wellbores (X01) for an integrated geomechanics study, focusing on profiling the stress across the Longmaxi and its adjacent formations. Combining geophysical logs and other stress indicators, we re-interpret its stress profile in the context of lithological variations. The resulting stress variations are modeled primarily through a viscoplastic stress relaxation framework, compared with the results via the frictional equilibrium and an elastic theory (the Extended Eaton model). We offer some discussions on the differences and similarities of these stress profiling methods, and examine their applicability to Longmaxi shale in the Changning area. Our objective is to connect the lithology-controlled stress variations to the first-order complexities (HF ineffectiveness and fault reactivation) that have been observed in the area to date.

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龙马溪页岩岩性控制应力变化——以长宁地区某评价井为例
龙马溪页岩是中国西南地区广泛、高产的非常规油气藏。长宁地区水力压裂增产效果不佳、断层再激活、套管损坏等因素影响了其开发。据推测,页岩储层内部和储层之间的应力对比关系到水力裂缝扩展和储层改造。为此,有必要对长宁地区龙马溪页岩地应力状态及其变化进行专门的定量研究。在这项研究中,我们重新访问了该区第一口评价井(X01)的现有数据,进行了综合地质力学研究,重点研究了龙马溪组及其邻近地层的应力剖面。结合地球物理测井和其他应力指标,在岩性变化的背景下重新解释了其应力剖面。与摩擦平衡和弹性理论(扩展伊顿模型)的结果相比,由此产生的应力变化主要通过粘塑性应力松弛框架进行建模。讨论了这些应力剖面方法的异同,并考察了它们在长宁地区龙马溪页岩中的适用性。我们的目标是将岩性控制的应力变化与迄今为止在该地区观察到的一阶复杂性(高频无效和断层再激活)联系起来。
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