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《Geotectonica Et Metallogenia》 2003-02
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STRUCTURAL CHARACTERISTICS IN THE NIUSHOUSHAN AREA, CENTRAL NINGXIA AND ITS GEOLOGICAL SIGNIFICANCE

ZHANG Jin1, MA Zong jin1, REN Wen jun2 and LEI Yong liang1 (1. School of Earth and Space Sciences, Peking University, Beijing 100871, China; 2. Department of Geophysical Survey, Changqing Oil Field Company, Wuzhong 751104, China)  
There are many thrust related structures developed in the Paleozoic strata of Niushoushan in the central Ningxia Hui Autonomous Region. The fault related folds are the typical structures in this area. Based on the analysis on these structures and their relationships, the processes which these structures of the Miboshan Formation were formed are reconstructured, and the strata have underwent about three stage deformation: (1) horizontal shortening; (2) folding and (3) thrusting. And it is proved that Niushoushan is the fore edge part of an old thrust sheet, the Niushoushan, the large Luoshan and the small Luoshan are the front part belt of this old thrust zone. So Niushoushan and the Ordovician in the central and southern Ningxia now are likely allochthons. From middle Ordovician to the Devonian, the areas of the central and southern Ningxia belong to the back arc foreland basin of North Qilianshan orogen, which are adjacent to the continent to the north. In the later early Paleozoic, with the closure of the back arc foreland basin, the Niushoushan was formed.
【Fund】: 国家自然科学基金(编号:4983402)项目资助.
【CateGory Index】: P548
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