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- W2355480982 abstract "The outcrops indicate that the unconformity boundaries exist in the interior of Nadu formation and between Nadu formation and Baigang formation of the Paleogene in Baise Basin. Based on the analysis of seismic data and well logs,the Nadu formation and Baigang formation of the Paleogene can be divided into one second-order sequence, and three third-order sequences. The member 3 of the Nadu formation forms sequence stratigraphy Ⅰ, the members 2 and 1 of the Nadu formation form sequence stratigraphy Ⅱ, and Baigang formation forms sequence stratigraphy Ⅲ. Sequence stratigraphy Ⅰ and Ⅱ are deposited during faulted period, and sequence stratigraphy Ⅲ is deposited during depreesion period. Sequence stratigraphy Ⅱ contains not only mudstonds of deep-lake subfacies with large thickness and wide distribution, but also rich sandstones of fluvial facies, fan delta facies, delta facies, and is the main sequence with source-reservoir-caprock assemblage combination. The sandstones of fan delta facies deposited in the north of the basin are available reservoirs. The long-axial widely distributed sandstones of fluvial facies and delta facies developed in the lowstand systems tract of each sequence are the potential reservoirs for hydrocarbon exploration of subtle traps." @default.
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- W2355480982 date "2005-01-01" @default.
- W2355480982 modified "2023-09-25" @default.
- W2355480982 title "Sequence stratigraphy and sedimentary evolution of Nadu formation and Baigang formation of the Paleogene in Baise Basin" @default.
- W2355480982 hasPublicationYear "2005" @default.
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