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《Geotectonica Et Metallogenia》 2004-01
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PALEOZOIC ARCUATE THRUST BELT IN CENTRAL AND SOUTHERN NINGXIA

ZHANG Jin1, MA Zongjin1, REN Wenjun2 and LEI Yongliang1 (1. School of Earth and Space Sciences, Peking University, Beijing 100871, Chi na; 2. Department of Geophysical Survey, Changqing Oil Field Company, Wuzhong 75 1104, China)  
In the period from Middle Ordovician to Devonian, the central and so uthern Ningxia area is the back-arc foreland basin in the north continental sid e of North Qilianshan orogen. In the late period of the Early Paleozoic, with th e closure of the back-arc foreland basin, a large arcuate thrust zone, broad in the west but narrow in the east, was produced in the study area, with the compr essive force originating from the southwest, namely, the North Qilian Orogen, wh ile the east-west trending structures in Weiningbeishan area are only parts of this salient. The Cenozoic arcuate structure was formed on the basis of the earl y one, but has changed the early one to certain extent.
【Fund】: 国家自然科学基金(编号:4983402)项目资助.
【CateGory Index】: P534
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