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- W2366714107 abstract "The sedimentary facies of some typical profiles as in Hancheng, Jiyuan, Denfeng, and Huainan and the characteristic of regional palaeogeography in the south of North China block were researched. The result shows that the research area had an evolution from epeiric sea to a lake basin during Palaeozoic to Triassic. This transition was controlled by the collision orogeny of Qinling orogenic belt directly.The collision began along the Shangnan Zhenping Tongbai line, making the south of North China block compressed and subsided, and transferred from a structural high land to an epeiric sea in Late Carboniferous. The west part of North Qinling began to uplift and became a source of terrigenous clastic sediments to North China basin. In the Perminan, the compression strengthened further and the North Qinling North Huaiyang structural belt uplifted, making the epeiric sea transit to a marginal lake basin. In the Triassic, the Qinling orogenic belt uplifted rapidly and the large scale depression lake basin developed in its north side, and the center of basin also transferred to the orogenic belt in the Late Triassic." @default.
- W2366714107 created "2016-06-24" @default.
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- W2366714107 date "2000-01-01" @default.
- W2366714107 modified "2023-09-26" @default.
- W2366714107 title "Sedimentary Tectonic Evolution from Late Palaeozoic to Triassic in the South of North China Block" @default.
- W2366714107 hasPublicationYear "2000" @default.
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