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Tectonic evolution of the Japanese island arc system
Taira, A
2001
Source PublicationANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES
ISSN0084-6597
Volume29Issue:xPages:109-134
AbstractGrowth 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.
KeywordAmurian Plate Motion Pacific-type Orogeny Baikal Rift-zone Northeast Japan Continental-crust Southwest Japan Superior Province Basin Development Hidaka Mountains Nankai Trough
Indexed BySCI
Language英语
Document Type期刊论文
Identifierhttp://ir.xtbg.org.cn/handle/353005/9848
Collection文献共享
Recommended Citation
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.
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