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- W2381761569 abstract "The Jurassic-Cretaceous stratum develops in Feixi area of Anhui Province,the north margin of the Dabie orogenic belt,where Middle-Upper Jurassic Yuantongshan Formation is about 1 170 m thick and mostly composed of fine detrital rocks.Based on Miall's classification of petrofacies,thirteen types of petrofacies are determined,which includes mainly Fl,Fm,Fr,Fsm,Sp,Sr,Ss and Sl,secondarily P,Frc,Sm,St and Sh,and five types of sedimentary facies are discriminated,which is comprised of point bar,floodplain,crevasse splay,shore and shallow lacustrine respectively.The deposit of Yuantongshan Formation goes through a bottom-up change from meandering deposit through shore-shallow lacustrine to meandering deposit system.The stream is a kind of fine highly bending meandering river,and it belongs to alluvial plain environment on the front of alluvial fans.It also reveals that Dabie orogenic belt as the source area of Yuantongshan Formation was in a far distant place and under stable tectonic setting in Middle-Late Jurassic." @default.
- W2381761569 created "2016-06-24" @default.
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- W2381761569 date "2011-01-01" @default.
- W2381761569 modified "2023-09-28" @default.
- W2381761569 title "Sedimentary characteristics of Middle-Upper Jurassic Yuantongshan Formation on northern margin of Dabie orogenic belt" @default.
- W2381761569 hasPublicationYear "2011" @default.
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