首页 | 本学科首页   官方微博 | 高级检索  
     检索      

The mapping methods and division of tectonic units of the regional tectonic map in the eastern China seas and adjacent regions
作者姓名:YIN Yanhong  ZHANG Xunhu  WEN Zhenhe  GUO Zhenxuan
作者单位:Qingdao Institute of Marine Geology, Qingdao 266071, China 
基金项目:The National Natural Science Foundation of China under contract No 40876033;;the foundation of Geological Investigation Bureau of China under contract No HY126-03
摘    要:The geological-geophysical map series of the eastern China seas and adjacent region (1:1 000 000) will be published in the late half year of 2009. The regional tectonic map is one of the main professional maps. The Mapping methods, the division method of geological tectonic units and the main geological tectonic units are mainly discussed. The strata from Pliocene to Holocene are peeled off so as to display the Pre-Pliocene structures. In basins, isopaches are drawn for the Cenozoic deposits. The plate tectonic theory and present tectonic pattern are adopted as the priorities in tectonic division. As to the division of intraplate tectonic units, it is a revision, complement and improvement of previous dividing systems, and the nomenclature for each tectonic unit follows the current system in China. The first-order tectonic unit is plate (Pacific Plate, Eurasian Plate and Philippine Sea Plate). The second-order tectonic unit is tectonic domain (East Asian continental tectonic domain,East Asian continental margin tectonic domain and west Pacific tectonic domain). The Philippine Sea Plate and the west part of the Pacific Plate are called the West Pacific tectonic domain. The part of the Eurasian Plate involved in this study area can be further divided into East Asian continental tectonic domain and East Asian continental margin tectonic domain. The East Asian continental margin domain is composed of the Ryukyu island arc, the Okinawa Trough back-arc basin and the back-arc basin of Sea of Japan. The East Asian continental tectonic domain in this study area is composed of the Sino-Korea Massif, the Changjiang River (Yangtze) Massif and South China Massif. In turn, these massifs consist of basins, folded belts or uplift zones. The basins,the folded belts or the uplift zones are further divided into uplifts and depressions made up of sags and swells.

关 键 词:构造单元划分  中国东部海域  映射方法  地质  邻区
收稿时间:5/4/2008 12:00:00 AM
修稿时间:2008/10/13 0:00:00

The mapping methods and division of tectonic units of the regional tectonic map in the eastern China seas and adjacent regions
YIN Yanhong,ZHANG Xunhu,WEN Zhenhe,GUO Zhenxuan.The mapping methods and division of tectonic units of the regional tectonic map in the eastern China seas and adjacent regions[J].Acta Oceanologica Sinica,2009,28(4):57-64.
Authors:YIN Yanhong  ZHANG Xunhu  WEN Zhenhe and GUO Zhenxuan
Institution:Qingdao Institute of Marine Geology, Qingdao 266071, China
Abstract:The geological-geophysical map series of the eastern China seas and adjacent region (1:1 000 000) will be published in the late half year of 2009. The regional tectonic map is one of the main professional maps. The Mapping methods, the division method of geological tectonic units and the main geological tectonic units are mainly discussed. The strata from Pliocene to Holocene are peeled off so as to display the Pre-Pliocene structures. In basins, isopaches are drawn for the Cenozoic deposits. The plate tect...
Keywords:regional tectonic map  eastern China seas  geological tectonic units  division  
本文献已被 CNKI 维普 万方数据 等数据库收录!
点击此处可从《海洋学报(英文版)》浏览原始摘要信息
点击此处可从《海洋学报(英文版)》下载免费的PDF全文
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号