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Tectonic implications of Late Paleozoic stratigraphic distribution in Northeast China and adjacent region

查看全文 作  者:ChengWen [1,2]Wang; YueWu [1,3]Sun; Ning [2]Li; GuoWei [3]Zhao;XiaoQin [2]Ma 高影响力作者 机构地区:[1] Key Laboratory for Evolution of Past Life and Environment in Northeast Asia under Ministry of Education, Jilin University, Changchun, 130026, China;[2] College of Earth Science, Jilin University, Changchun, 130061, China;[3] Research Center of Paleont高影响力机构 出  处:《Science China Earth Sciences》索引2009年第52卷第5期,共8页高影响力期刊 基  金:Supported by Science and Technology Project of Sinopec (Grant No. G0800-06-ZS-324) 1) Mineral Resources Authority of Mongolia. Geological Map of Mongolia (1:1000000), Ulaanbaatar. 1998 2) Kociurzhinskim B V, Poliakovym V M, Efriemovoii V N. Geological Map of Chita (1:1000000), Russia. 20003) Krasnyi L I, Peng Y B. Geological Map of Amur Region and Adjacent Areas (Scale 1:2500000), Harbin, China. 1996 摘  要:An analysis of the distribution of the Late Paleozoic strata on Northeast China and adjacent region reveals a zonal pattern of the distribution around the core of the Jiamusi-Mongolia Block.The main part of Late Paleozoic marine strata in this area is considered the continental margin deposits of the Jia-musi-Mongolia Block by analyzing the stratigraphic contact relationship,lithofacies,etc.The results are exhibited in a series of tectonic paleogeographic maps.This presents an important proof for the foundation of the Jiamusi-Mongolia Block,and confines the forming time of Jiamusi-Mongolia Block to the Late Silurian. 关 键 词:Northeast China and ADJACENT area Late PALEOZOIC STRATA tectonic paleogeographic character Jiamusi-Mongolia Block
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