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- W2384678691 abstract "The black shale in Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation of Sichuan Basin is one of the important target strata for shale gas exploration.Based on the analysis by various methods,this paper studies the mudstone(shale)profile of Upper Ordovician Wufeng Formation-Lower Silurian Longmaxi Formation in Qilong village,Xishui County in the southeast of Sichuan Basin.The cracks(joints)of the profile are coincident with the regional faults.There are three groups of strikes(nearly E-W,NWW and NEE trend)and S-N trend in the profile.The fractures in the shale reservoirs exist in the form of microcracks.Along with the increase of the compressive strength,the microcracks of the rocks are also damaged seriously and gradually form a large-scale and complex fracture network system.The rock mechanics properties of the parallel beddings are mainly controlled by the ground stress.If the hydraulic fractures are perpendicular to the maximum horizontal stress(SWW trend)direction,the hydraulic fracturing area will be expanded." @default.
- W2384678691 created "2016-06-24" @default.
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- W2384678691 date "2013-01-01" @default.
- W2384678691 modified "2023-09-26" @default.
- W2384678691 title "Fracture characteristics of shale in Upper Ordovician-Lower Silurian in Xishui area,southeast of Sichuan Basin,China" @default.
- W2384678691 hasPublicationYear "2013" @default.
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