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中国的榴辉岩
引用本文:徐少康. 中国的榴辉岩[J]. 化工矿产地质, 2004, 26(4): 193-204
作者姓名:徐少康
作者单位:中化地质矿山总局地质研究院,河北,涿州,072754
摘    要:自20世纪90年代,对中国大别山造山带等地榴辉岩的研究,已成为国际地学界关注的热点。榴辉岩形成于高一超高压地质环境,其分布、地质产状、矿物组合、地球化学特征、成岩温压、成岩年龄及相关矿产等具有自身的特点,对其成因尚有地幔捕获说、岩浆说、变质说等不同认识。

关 键 词:榴辉岩  高-超高压变质作用  大别山
文章编号:1006-5296(2004)04-0193-12
修稿时间:2004-06-17

CHINESE ECLOGITE
Xu Shaokang Geology Institute of China Chemical Geology , Mining Bureau,Zhuozhou,Hebei,,China. CHINESE ECLOGITE[J]. Geology of Chemical Minerals, 2004, 26(4): 193-204
Authors:Xu Shaokang Geology Institute of China Chemical Geology & Mining Bureau  Zhuozhou  Hebei    China
Affiliation:Xu Shaokang Geology Institute of China Chemical Geology & Mining Bureau,Zhuozhou,Hebei,072754,China
Abstract:Since the nineties of the 20th century,the research to the eclogite in the place,such as Dabieshanorogenic zone of China,etc.have become geoscience circle internationally pay attention to hot point.eclogiteformed in the geological environment of high pressure-superhigh pressure,its distribute,geologicaloccurrence,mineral association,the characteristic of geochemistry,diagenetic temperature and press,diagenetic age and related minerals etc.Have the characteristic of self,but about its original have mantlecapture hypothesis,magma hypothesis,mteamorphism hypothesis etc.different hypothesis
Keywords:eclogite  high pressure-superhigh pressure mteamorphism  Dabieshan mountain
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