CHARACTERISTICS OF THE TECTONIC FRAMEWORK OF NORTHEAST ASIAN MESOZOIC ACTIVE CONTINENTAL MARGIN
ZHANG Yun-ping1,2, SONG Wei-min1,3, NA Fu-chao1, BAO Qing-zhong1, WANG Yan1
1. Shenyang Institute of Geology and Mineral Resources, CGS, Shenyang 110034, China; 2. Development and Research Center, CGS, Beijing 100037, China; 3. Graduate School, Northeastern University, Shenyang 110004, China
Abstract：Northeast Asia is one of the most complex areas of plate tectonic activities in the world. The eastern continental margin accretion zone involves two types, i.e., collisional orogenic belt and accretionary orogen belt. The western margin reactivation zone contains Eastern Siberia ancient land reactivation region (north), East Mongolia-Xing'an-Jihei reactivation region (middle), and eastern Sino-Korea ancient land reactivation region (south). The overall structural framework of the Northeastern Asian Mesozoic active continental margin is characterized by zonation from east to west, segments from north to south, and development from northeast to south. The late Middle Jurassic-early Early Cretaceous sedimentary-volcanic-sedimentary molasse in North China-Mongolia-Xing'an Region, which is a component part of the Northeast Asian Mesozoic activite continental margin in its evolutionary process, is one of the indicators of tectonic system transition.
张允平, 宋维民, 那福超, 鲍庆中, 汪岩. 东北亚活动大陆边缘中生代构造格架主体特点[J]. 地质与资源, 2016, 25(5): 407-423.
ZHANG Yun-ping, SONG Wei-min, NA Fu-chao, BAO Qing-zhong, WANG Yan. CHARACTERISTICS OF THE TECTONIC FRAMEWORK OF NORTHEAST ASIAN MESOZOIC ACTIVE CONTINENTAL MARGIN. GEOLOGY AND RESOURCES, 2016, 25(5): 407-423.
2016, Vol. 25 
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