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- W2369834443 abstract "Paleo-climate is the major factor that decides the type of reservoir space and the moving pathway in carbonate oil-gas pool.Rift and cavity are the characteristic productions of the Ordovician carbonate rock under the moist paleo-environment in Tarim basin.Based on geologic investigations on corrosion zone in weathered mantle,the fractures are divided into 2 types according to the origin,and four stages according to the structural developing history,as well as three grades according to the scale.And the developing characteristics of the paleo-cavity are illustrated also.It is indicated that rift and cavity don't distribute lonely.Actually,cavity and its surrounding regions constitute an integrated rift-cavity system.So,the heterogeneous karst distribution pattern of carbonate reservoir in fossil weathered mantle,structure pattern of rift-cavity oil-gas pool,is built by combined rift and cavity.At last,oil unit,namely the region where rift and cavity are centralized relatively and connect to each other,is put forward for the research on understanding the substance of the riftcavity oil-gas pool." @default.
- W2369834443 created "2016-06-24" @default.
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- W2369834443 date "2006-01-01" @default.
- W2369834443 modified "2023-09-25" @default.
- W2369834443 title "STRUCTURE PATTERN OF RIFT-CAVITY OIL-GAS POOL IN CARBONATE ROCK UNDER MOIST PALEO-ENVIRONMENT —A Case Study on the Ordovician in Tarim Basin" @default.
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