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《Geology in China》 2010-04
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Tectonic framework and main characteristics of North China and its northward areas in Late Paleozoic-Early Mesozoic period

ZHANG Yun-Ping,LI Jing-Chun(Shenyang Institute of Geology and Mineral Resources,CGS,Shenyang 110034,Liaoning,China)  
A comparative study of geotectonic cycles and evolution characteristics of the tectonic domain from the Atlantic Ocean to Paleo-Asia Ocean on the global scale is beneficial to understanding the regional tectonic evolution of the giant tectonic domain.The establishment of the concept of "dynamic behaviors" of the attributes of paleocontinents tectonic units and the correlation analysis of the composite orogenic area and its neighboring tectonic units have revealed that the formation and development of the North China foreland basin were closely related to the tectonic evolutionary process of the neighboring composite orogenic area.In North China and its northward areas,Late Paleozoic-Early Mesozoic tectonic framework has the following features:1)In the Mongolian-Da Hinggan composite orogenic area,Paleozoic fold belts were interwoven with intermediate massifs,leading to the development of the epicontinental sea basin and the aulacogen and superposed basins during the Carboniferous-Permian period and the inter-mountainous basin during the Triassic period,based on the fold belt of the earlier stage.2)The foreland basin in North China was developed synchronically with the tectonic evolution process of the northern composite orogenic area and formed the marine facies,marine-continental interaction sediments on the old land during the Carboniferous period and the continental facies sediments during the Permian-Middle Triassic period,characterized by red bed and gypsum salt in local areas.3)The "tectonomagmatic activation belt" on the North China continental margin in the Late Paleozoic?Early Mesozoic period was the southernmost tectonic unit of the Mongolian-Da Hinggan composite orogenic area.
【Fund】: 中国地质调查局地质大调查项目(1212010610511 1212010813032)资助
【CateGory Index】: P542
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10 WANG Shi-jin1,WAN Yu-sheng2,ZHANG Cheng-ji3,YANG En-xiu1,SONG Zhi-yong1,WANG Li-fa1,ZHANG Fu-zhong1(1.Shandong Geological Survey Institute,Shandong Jinan 250013,China;2.Beijing Ion Probe Center,Beijing,100037 China;3.Shandong Exploration Bureau of Geology and Mineral REsources,Shandong Jinan 250013,China);Major Advanced Developement Gained in Studying Early Cambrian Geology in Luxi Area[J];山东国土资源;2008-01
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