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- W2378622128 abstract "The Quaternary of Qaidam basin, being lack of topographic break, was studied based on the theory of sequence stratigraphy, which originated from marine basins in passive continental margin. Through comprehensive researches on outcrops, cores, well logging and seismic data, the Quaternary of Qaidam basin was divided into five sequences. The distinct characteristics of sequence boundary and maximum flooding surface have been identified. The sedimentary sequence in a continental basin, which is lack of topographic break, only consists of lower trangressive system tract and upper regressive system tract. Trangressive system tract is composed of several retrogradation parasequence sets, its sand shale ratio is decreasing upward; regressive system tract mostly consists of prograded parasequence sets, its sand shale ratio is increa sing downward. The former was formed during moist climate with much material feeding and developed good source rock and reservoirs of delta and beach bar. The latter was formed during arid season with less material feeding and constituted good caps of mudstone and salt." @default.
- W2378622128 created "2016-06-24" @default.
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- W2378622128 date "2002-01-01" @default.
- W2378622128 modified "2023-09-23" @default.
- W2378622128 title "Quaternary sequence stratigraphy and hydrocarbon evaluation in Qaidam basin" @default.
- W2378622128 hasPublicationYear "2002" @default.
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