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四川挖角坝地区辉绿岩脉岩石学特征及成因研究
引用本文:夏廷高,孙传敏,尹建忠.四川挖角坝地区辉绿岩脉岩石学特征及成因研究[J].地质与勘探,2005,41(4):57-61.
作者姓名:夏廷高  孙传敏  尹建忠
作者单位:1. 成都理工大学地球科学学院,成都,610059;四川省冶金地质勘查局,成都,610081
2. 成都理工大学地球科学学院,成都,610059
摘    要:扬子地台西缘与松潘-甘孜造山带东缘结合部的挖角坝地区,发育了一系列基性岩墙群,对其代表性岩脉的岩相学、矿物学、岩石化学等进行了研究,分析认为基性岩脉可能来源于富集地幔、并在上升过程中有一定量地壳物质的混入.

关 键 词:辉绿岩脉  岩石学特征  成因研究  挖角坝
文章编号:0495-5331(2005)04-0057-05
收稿时间:2004-04-06
修稿时间:2004年4月6日

THE STUDY OF DIABASE VEIN PETROLOGY CHARACTER AND PETROGENESIS IN WAJIAOBA REGION OF SHIMIAN COUNTY SICHUAN PROVINCE
XIA Ting-gao,SUN Chuan-min,YIN Jian-zhong.THE STUDY OF DIABASE VEIN PETROLOGY CHARACTER AND PETROGENESIS IN WAJIAOBA REGION OF SHIMIAN COUNTY SICHUAN PROVINCE[J].Geology and Prospecting,2005,41(4):57-61.
Authors:XIA Ting-gao  SUN Chuan-min  YIN Jian-zhong
Abstract:Basic rock dyke group in the Wajiaoba region, which lies in the junction position of the western edge of Yangtze platform and the eastern fringe of Songpan-Ganzi orogenic belt, is chosen to study. Petrography, mineralogy and petrochemistry of representative basic rock dykes are discussed. It is concluded that this basic rock dyke group originates from enrichment mantle, and is mixed with some Earth's crust substance during ascending process.
Keywords:diabase dyke  petrology  petrogenesis  Wajiaoba
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