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- W2355221570 abstract "Based on the basic principles of sequence stratigraphy and sedimentology, two measured sections of the Jingmen-Dangyang Basin were studied for sedimentary facies analysis and sequence stratigraphic division. Furthermore, facies transformation discipline, sequence boundaries and stratal stacking patterns and the dominating factors were also studied. The research indicates the upper Triassic can be divided into four third-order sequences, such as TS1, TS2, TS3 and TS4. The unconformity, lithology and lithofacies transition surface and river erosion surface are the main sequence boundaries. From TS1-TS2 to TS3-TS4, Jingmen-Dangyang Basin experiences the transformation from the lacustrine to the fluvial depositional system, which represents the initial characteristics of the northern Yangtze foreland basin. The Jiuligang Formation is characterized by the thin-substrate coal-bearing sedimentary cycles of lake and swamp facies, indicating an inadequate provenance. In contrast, the Wanglongtan Formation is composed of a series of thick-substrate sandstone dominated cycles, it presents intensification of structural activities and super-saturation of the basin." @default.
- W2355221570 created "2016-06-24" @default.
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- W2355221570 date "2009-01-01" @default.
- W2355221570 modified "2023-10-02" @default.
- W2355221570 title "Research on Outcrop Sequence Stratigraphy of Upper Triassic in Jingmen-Dangyang Basin" @default.
- W2355221570 hasPublicationYear "2009" @default.
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