Advances in research of Asian geology-A summary of 1:5M International;Geological Map of Asia project
Ren, Jishun2; Niu, Baogui; Wang, Jun; Jin, Xiaochi; Zhao, Lei; Liu, Renyan
刊名JOURNAL OF ASIAN EARTH SCIENCES
2013
卷号72;SI SI页码:3-11
关键词IGMA5000 Volcanics Granite Composite continent Pangea reconstruction Indosinian foldbelt
ISSN号1367-9120;EI 1878-5786
DOI10.1016/j.jseaes.2013.02.006
英文摘要The International Geological Map of Asia at a 1:5,000,000 scale (IGMA5000) is the first digital Asian geological map under the standard of the Commission for the Geological Map of the World (CGMW). Major advances that have been achieved in compiling the map are manifested in the following understandings.;(1) Large amounts of Mesozoic volcanic rocks occurring in the eastern Asian coastal area are mainly Cretaceous instead of Upper Jurassic-Lower Cretaceous. Most of the Carboniferous-Permian volcanic rocks in Central Asia seem not to be arc volcanics, but the product of an extensional stage. The basal boundary of the Meso-Neoproterozoic Jixian section in China is not dated at 1.8 Ga as defined previously, but less than 1.68 Ga.;(2) The most significant Neoarchean tectono-thermal events in the Sino-Korean craton and the Indian craton took place at 2.5 Ga rather than at 2.7 Ga. The basement of the Yangtze craton was finally formed at 0.75-0.8 Ga, which is 0.2-0.3 Ga later than the Greenville orogenic cycle. Geologically, South China is identified to be an Early Paleozoic Caledonian foldbelt. The Qinling belt, where no oceanic basin was developed in Triassic times, is not an Indosinian collisional orogen, but a continental crust subduction one. When Pangea was formed, Indo-Australian Gondwana had been joined to Paleo-Asia and between them there was no oceanic basin, i.e. no Paleo-Tethys which continued from Paleozoic to Mesozoic. A huge Indosinian orogenic belt existed on the southern margin of Paleo-Asia to the north of the Zagros-Himalayas.;(3) Asia is a composite continent consisting of three major cratons-the Siberian, Indian and Arabian and three huge orogenic belts with a number of minor cratons and numerous microcontinents included. The main body of the Asian continent took its shape during the Mesozoic. The orogenic belts belong respectively to three global tectonic domains: the Paleo-Asian, Tethyan and Pacific. The small cratons, such as Sino-Korea, Yangtze, Tarim, and Sibumasu are thought to be affiliated to the tectonic transform zone between Gondwana and Siberia. They had been situated on the northern margin of Gondwana before the disappearance of the Paleo-Asian Ocean, and were lying on the southern margin of Paleo-Asia after the closing of the Paleo-Asian Ocean and then the opening of the Tethys. The fact that ophiolites in Asia appear to get progressively younger in age from north to south throws light on the Phanerozoic evolutionary process of the dispersion of Gondwana and the accretion of Asia accompanied by a southward migration of its orogenic belts. (c) 2013 Elsevier Ltd. All rights reserved.
学科主题地质普查勘探方法
WOS关键词CARBONIFEROUS VOLCANIC-ROCKS ; TECTONIC EVOLUTION ; NW CHINA ; CRUSTAL ; STRUCTURE ; WESTERN TIANSHAN ; MAGMATIC ROCKS ; NE CHINA ; MARGIN ; BELT ; IRAN
WOS研究方向Geology
语种英语
出版者PERGAMON-ELSEVIER SCIENCE LTD
WOS记录号WOS:000321404900002
内容类型期刊论文
源URL[http://119.78.100.197/handle/2HKVOGP0/40097]  
专题中国地质科学院地质研究所
作者单位1.Chinese Acad Geol Sci, Inst Geol, Beijing 100037, Peoples R China.
2.中国地质科学院地质研究所
推荐引用方式
GB/T 7714
Ren, Jishun,Niu, Baogui,Wang, Jun,et al. Advances in research of Asian geology-A summary of 1:5M International;Geological Map of Asia project[J]. JOURNAL OF ASIAN EARTH SCIENCES,2013,72;SI SI:3-11.
APA Ren, Jishun,Niu, Baogui,Wang, Jun,Jin, Xiaochi,Zhao, Lei,&Liu, Renyan.(2013).Advances in research of Asian geology-A summary of 1:5M International;Geological Map of Asia project.JOURNAL OF ASIAN EARTH SCIENCES,72;SI SI,3-11.
MLA Ren, Jishun,et al."Advances in research of Asian geology-A summary of 1:5M International;Geological Map of Asia project".JOURNAL OF ASIAN EARTH SCIENCES 72;SI SI(2013):3-11.
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