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- W2364755645 abstract "The paleoenvironment of Jurassic in the southeastern Tarim basin was reconstructed based on the analysis of depositional and seismic facies.The results indicate that the depositional systems were consisted of alluvial-fan,braided-river delta at the early period of early Jurassic.From the later period of early Jurassic to the early period of middle Jurassic,the braided-river delta and littoral-shallow lake developed in this area.During the middle period of middle Jurassic,the depositional environment was mostly composed of lakes and rivers.At the late period of middle Jurassic,the lakes started to recess.The subsidence center of Jurassic was located in Altun.The southeastern Tarim,the western Qaidam basin and Tula basin were joined together at early-middle Jurassic,which are different compositional parts of the same continental basin at the foothill of Kunlun.The current distribution of Jurassic is resulted from thrust-uplifting of Altun mountain and slip-displacing of Altyn tagh fault." @default.
- W2364755645 created "2016-06-24" @default.
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- W2364755645 date "2008-01-01" @default.
- W2364755645 modified "2023-09-25" @default.
- W2364755645 title "Jurassic Sedimentary Facies and Paleoenvironmental Reconstruction of Southeastern Tarim Basin,Northwestern China" @default.
- W2364755645 hasPublicationYear "2008" @default.
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