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- W2374097410 abstract "Jinhua-QuzhouBasin developed on the metamorphosed basement of Palaeozoic fold, and its formation and development was greatly influenced by pre-mesozoic tectonic framework and geological characteristics. In this paper, the author studied paleogeographic environment, sedimentary structure, depocenter and paleolithological changes etc., analyzed Jinhua-Quzhou Basin's history of formation and evolution and discussed its evolution of tectonic setting from Late-Mesozoic to Cenozoic. From what was studied, four conclusions have been reached: ①Jinhua-Quzhou basin was a fault basin because of compression and then extention; and its boundaries were mostly normal faults. ②In different areas of the basin, there were different stratigraphic sequences. ③Sedimentary facies: the distribution of Jinhua-Quzhou Basin's sedimentary facies varied in different stages, and to some extent, the evolution sequences were clear. Alluvial fan facies spread in northern and southern borders of Jinhua-Quzhou basin as alluvial fan apron with some differences. River facies and sand bank facies distributed in the middle of Jinhua-Quzhou Basin, locating in sectors between Quxian and Longyou. Delta facies included fan delta, braided delta and normal delta. Also, in areas we studied, there were lake facies, but shore shallow lake subfacies and semi-deep lake subfacies were the most important ones." @default.
- W2374097410 created "2016-06-24" @default.
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- W2374097410 date "2004-01-01" @default.
- W2374097410 modified "2023-09-27" @default.
- W2374097410 title "Sedimentary Facies and Evolution of Tectonic Environments in the Jinhua-Quzhou Basin,Zhejiang Province" @default.
- W2374097410 hasPublicationYear "2004" @default.
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