Tectonic evolution of the Japanese island arc system

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	Tectonic evolution of the Japanese island arc system
	Taira, A
刊名	ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES
	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
内容类型	期刊论文
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
推荐引用方式 GB/T 7714	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.