朝鲜半岛地质与东北亚构造演化:前言

发布时间：2018-06-15 05:33

本文选题：朝鲜半岛 + 构造演化　；参考：《岩石学报》2016年10期

【摘要】：正【岩石学报】2016年10月第32卷第10期是朝鲜半岛与东北亚构造演化专辑。朝鲜半岛处于东北亚的欧亚大陆与太平洋的交界地区。东边毗邻作为岛弧带的日本,西部与我国辽吉接壤,是欧亚大陆的东部边界(图1)。其基底陆块全部或部分与华北相连。它的显生宙演化又记录了与古亚洲洋(含鄂霍茨克海)演化、古特提斯演化、Pegea超大陆的形成以及古太平洋和西太平洋板块运动的各种地质事件,是研究东北亚以至全球构造的关键地区。由于众所周知的国际政治原因,朝鲜的地质情况,特别是新的研究进展公开发表的不多。从1996年起,朝鲜国家科学院
[Abstract]:October, 2016 Volume 32 No. 10 is the album of tectonic Evolution of the Korean Peninsula and Northeast Asia. The Korean peninsula is located in Northeast Asia's Eurasia and Pacific Ocean border area. Japan is adjacent to Japan as an island arc belt to the east and Liao Ji to the west of China. It is the eastern boundary of Eurasia (fig. 1). Its basement land block is connected with North China in whole or in part. Its Phanerozoic evolution also recorded various geological events related to the evolution of the Paleo-Asian Ocean (including the Okhotsk Sea), the formation of the PaleoTethys supercontinent and the paleo-Pacific and western Pacific plate movements. Is the study of Northeast Asia and even the global structure of the key region. Due to well-known international political reasons, the geology of North Korea, especially the new research progress, has not been published. Since 1996, the National Academy of Sciences of the DPRK
【作者单位】：中国科学院地质与地球物理研究所;大陆动力学国家重点实验室西北大学;
【分类号】：P542

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