METAMORPHIC BELTS OF JAPANESE ISLANDS

被引：47

作者：

BANNO, S ^{[1
]}

NAKAJIMA, T ^{[1
]}

机构：

[1] GEOL SURVEY JAPAN,DEPT GEOCHEM,TSUKUBA 305,JAPAN

来源：

ANNUAL REVIEW OF EARTH AND PLANETARY SCIENCES | 1992年 / 20卷

关键词：

HIGH-PRESSURE METAMORPHISM; LOW-PRESSURE METAMORPHISM; PAIRED METAMORPHISM; ISLAND ARC;

D O I：

10.1146/annurev.ea.20.050192.001111

中图分类号：

P1 [天文学];

学科分类号：

0704 ;

摘要：

The Japanese islands are composed of many metamorphic belts. Most of them were derived from late Paleozoic to Cenozoic accretionary complexes which develoepd along the eastern border of the Asian continent. They are either andalusite-sillimanite type, low-pressure metamorphic belts, or intermediate high-pressure belts where epidote + glaucophane and locally aragonite are stable. Besides metamorphic belts consisting of a single metamorphic unit, there are regions where small areas and blocks of various metamorphic rocks are abundant within serpentinite and sedimentary sequences. -from Authors

引用

页码：159 / 179

页数：21

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