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- W2364509056 abstract "By comparing and analyzing the lithology,the seismic reflection fabric and the sequence development characteristics between and Dongrong Formation in Suibin depression,it is found that the lithology of the lower part of and Dongrong Formation are sandy conglomerate and conglomerate;the middle part are mainly of fine sandstone and siltstone;the upper part sediments all includes volcanic rocks.Didao includes coal bed,but Dongrong Formation does not.In seismic profile the amplitude and continuity of Dongrong Formation are better than Formation.Both and Dongrong Formation experience twice sea level changes in sequence development process and they have pertinence.It is marine sediments of Dongrong Formation in northeast of Suibin depression and in the southwest is fan delta lake sediments.So the author considers that should be included in Dongrong Formation,and it is heteropical deposits of Dongrong Formation and hereby indicates that Didao and Dongrong Formation have well source rock-reservoir-cap combination." @default.
- W2364509056 created "2016-06-24" @default.
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- W2364509056 date "2007-01-01" @default.
- W2364509056 modified "2023-09-23" @default.
- W2364509056 title "Study on Stratum and Sedimentary Facies of Didao Formation and Dongrong Formation in Suibin Depression of Sanjiang Basin" @default.
- W2364509056 hasPublicationYear "2007" @default.
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