中国科学院机构知识库网格
Chinese Academy of Sciences Institutional Repositories Grid
Tectonic evolution of the Japanese island arc system

文献类型:期刊论文

作者Taira, A
刊名ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES
出版日期2001
卷号29期号:x页码:109-134
关键词AMURIAN PLATE MOTION PACIFIC-TYPE OROGENY BAIKAL RIFT-ZONE NORTHEAST JAPAN CONTINENTAL-CRUST SOUTHWEST JAPAN SUPERIOR PROVINCE BASIN DEVELOPMENT HIDAKA MOUNTAINS NANKAI TROUGH
ISSN号0084-6597
中文摘要Growth of the Japanese are system, which has mainly taken place along the continental margin of Asia since the Permian, is the result of subduction of the ancient Pacific ocean floor. Backarc basin formation in the Tertiary shaped the present-day are configuration. The neotectonic regime, which is characterized by strong east-west compression, has been triggered by the eastward motion of the Amur plate in the Quaternary. The tectonic evolution of the Japanese are system includes formation of rock assemblages common in most orogenic belts. Because the origin and present day tectonics of these assemblages are better defined in the case of the Japanese are system, study of the system provides useful insight into orogenesis and continental crust evolution.
收录类别SCI
原文出处10.1146/annurev.earth.29.1.109
语种英语
公开日期2016-05-12
源URL[http://ir.xtbg.org.cn/handle/353005/9848]  
专题西双版纳热带植物园_文献共享
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Taira, A. Tectonic evolution of the Japanese island arc system[J]. ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES,2001,29(x):109-134.
APA Taira, A.(2001).Tectonic evolution of the Japanese island arc system.ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES,29(x),109-134.
MLA Taira, A."Tectonic evolution of the Japanese island arc system".ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES 29.x(2001):109-134.

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来源:西双版纳热带植物园

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