Study on Law of Structural Evolution and Sedimentary Evolution for North Uskyurt Basin

Chao Liu; Hai Tao Xue; Shuang Wang; Yu Jiao Sun

doi:10.4028/www.scientific.net/AMR.671-674.302

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HomeAdvanced Materials ResearchAdvanced Materials Research Vols. 671-674Study on Law of Structural Evolution and...

Study on Law of Structural Evolution and Sedimentary Evolution for North Uskyurt Basin

Abstract:

North Uskyurt Basin, located on Turan Plain, northwestern Central Asian, is continental polycyclic cratonic. The structural evolution of the basin underwent six phases: basement formulation, passive edge, rifting, post-rifting, compression, early Neogene depression. Regional structural evolution takes control of complicated transition of North Uskyurt sedimentary structure. In general, basin sedimentary environment underwent basement (granite, metamorphic rocks) passive edge, late Devonian epoch carboniferous period (marine facies) rifting, late Permian epoch-triassic period (continental facies) post-rifting, Jurassic period-Cretaceous period (Marine-continental Transition Facies, marine facies) compression, late Eocene-Miocene epoch (marine-continental facies coexistence) Neogene depression, Pliocene-Holocene (continental facies). Consequently, sedimentary formation in which various sedimentary environment, such as marine facies, continental facies, are coexisted with various rock types, such as clastic rocks, carbonate rocks, is generated.

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Periodical:

Advanced Materials Research (Volumes 671-674)

Pages:

302-305

DOI:

https://doi.org/10.4028/www.scientific.net/AMR.671-674.302

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Online since:

March 2013

Authors:

Chao Liu, Hai Tao Xue, Shuang Wang, Yu Jiao Sun

Keywords:

North Uskyurt Basin, Sedimentary Evolution, Structural Evolution

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References

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