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《Chinese Journal of Geology》 1978-01
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ON THE FEATURES OF TURBIDITE SEQUENCES IN SOME REGIONS OF CHINA

Li Jiliang, Chen Changming, Gao Wenxue, Chen Ruijun, Huang Jiakuan, Tian You'xing and Liu Jiehan  
Turbidite sequences are developed in strata of Lower Tertiary of North-East China, Trias of Qin Ling and Upper Ordovician of West Zhejiang Province. In this study, the sedimentary structures, textures, petrographic features, petrochemistry and other characteristics are analyzed. Based on these analyses, it can be assumed that the turbidite-bearing basins belong to a sort of marginal basins originated by extension at different times. The Tertiary turbidite basin of North-Bast China was initially extended about 46 m.y. ago with the extrusion of basalt, being a transitional member from alkaline basaltic to tholeiitic series. Following this, thick turbidite sequence was deposited. In the basin mollass sequence was developed subsequently and the basin has been subjected to contract by compressive action. The Trias and Ordovician turbidite basins are developed on basements composed of carbonate terrains, and formed by extention. Along these lines of evidence the tectonic history is restored.
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