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《成都地质学院学报》 1993-01
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SEDIMENTARY CHARACTERISTICS AND EVOLUTION OF EARLY ORDOVICIAN IN ORDOS BASIN

Li Anren Liu Wenjun Zhang Jinquan Geng Aiqin Hao Shuming  
Ordos Basin located at the western margin of Huabei plateform in the early Paleozoic. In this area, depositional environment could be divided into three different divisions during Early Ordovician: a distally steepened carbobnate ramp in western depositional division ;an accretional rimmed carbonate platform in southern depositional division and a evaporite-restricted platform in eastern depositional division. In the evolution of the lithofacies and paleogeography of lower Ordovician in Ordos Basin three stages can be recognized: (1) stable stage (Yeli-Liangjiashan epoch); (2) differentiation stage(early-late Majiagou epoch); (3) early episode of the evolution of deepwater basin with clastic turbidite in Middle Ordovician (Fengfeng epoch). The structural development of the basin is characteried by uplifting in eastern division and descending in western division (upward shallowing sequence in the eastern division, upward deepening sequence in the western division).
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