THE MESO-NEOPROTEROZOIC TECTONO-STRATIGRAPHIC DIVISION ON THE EPICONTINENTAL MOBILE BELT IN NORTHERN LIAONING PROVINCE
GUO Wei-jing1, LI Jun-jie2, WU Ying-jie3
1. Liaoning Institute of Geological Survey, Dalian 116100, Liaoning Province, China; 2. Shenyang Institute of Geology and Mineral Resources, Shenyang 110033, China; 3. Liaoning Vocational College of Finance, Shenyang 110122, China
Abstract：There exists a series of Meso-Neoproterozoic tectonic melanges and ophiolitic melanges in Jianping-Fuxin-Tieling area of northern Liaoning Province. Their original rocks are volcanic rocks, epicontinental clastic sedimentary rocks, and ophiolite of volcanic and island arc tholeiitic series or calcium alkali series. The rocks coexist closely, distributing in a narrow and long belt in the Late Precambrian orogenic belt in northern Liaoning. The rock series could be subdivided into Weijiagou rock group and Kaiyuan rock group (including Shenjiapuzi rock formation, Zhaobeishan rock formation and Banshigou rock formation).
郭伟静, 李俊杰, 吴英杰. 关于辽宁北部陆缘活动带中新元古代构造地层划分[J]. 地质与资源, 2006, 15(4): 241-246.
GUO Wei-jing, LI Jun-jie, WU Ying-jie. THE MESO-NEOPROTEROZOIC TECTONO-STRATIGRAPHIC DIVISION ON THE EPICONTINENTAL MOBILE BELT IN NORTHERN LIAONING PROVINCE. GEOLOGY AND RESOURCES, 2006, 15(4): 241-246.
2006, Vol. 15 
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