| 注册
首页|期刊导航|岩石矿物学杂志|关于C型埃达克岩成因的再探讨

关于C型埃达克岩成因的再探讨

张旗

岩石矿物学杂志2011,Vol.30Issue(4):739-747,9.
岩石矿物学杂志2011,Vol.30Issue(4):739-747,9.

关于C型埃达克岩成因的再探讨

Reappraisal of the origin of C-type adakitic rocks from East China

张旗1

作者信息

  • 1. 中国科学院地质与地球物理研究所,北京100029
  • 折叠

摘要

Abstract

A comprehensive summary of the definition, mode of occurrence and remaining problems in the studies of C-type adakitic rocks is given in this paper for better understanding the implications of C-type adakite rocks in East China. It is pointed out that C-type adakitic rocks are high-K calc-alkaline and are likely derived from partial melting of intermediate- to high-K meta-andesitic-basaltic rocks under the high pressure condition. Unlike things of O-type adakite, the origin, source rocks and partial melting processes of C-type adakite remain unclear and hence more experimental work may have to be involved in future work.

关键词

C型埃达克岩/O型埃达克岩/成因/意义

Key words

C-type adakite/O-type adakite/origin/implications

分类

天文与地球科学

引用本文复制引用

张旗..关于C型埃达克岩成因的再探讨[J].岩石矿物学杂志,2011,30(4):739-747,9.

基金项目

国家自然科学基金重大研究计划资助项目(91014001,90714011,90714007) (91014001,90714011,90714007)

中国科学院地质与地球物理研究所岩石圈演化国家重点实验室自主研究课题资助项目(专0904) (专0904)

岩石矿物学杂志

OA北大核心CSCDCSTPCD

1000-6524

访问量0
|
下载量0
段落导航相关论文