首页 | 本学科首页   官方微博 | 高级检索  
     检索      

豫西南许窑沟金矿成因
引用本文:常秋玲,卢欣祥,薛青.豫西南许窑沟金矿成因[J].黄金地质,2002,8(3):38-42.
作者姓名:常秋玲  卢欣祥  薛青
作者单位:1. 河南省地质科学研究所,河南,郑州,450053
2. 河南省南阳市黄金管理局,河南,南阳,473056
摘    要:对许窑沟金矿产出的地质背景,矿床特征,控矿因素及矿床成因等几方面作了系统的论述,提出了断裂,特别是韧性剪切带对成矿的主要控制作用;花岗岩与成矿有较大的时差,具有穿时,穿层的特点,它起着沟通深部与浅部的作用,并使深部的含Au流体沿断裂破碎带上升,沉淀而成矿。

关 键 词:金矿床  成矿流体  成矿机理  控矿因素  韧性剪切带  河南  花岗岩
文章编号:1006-558X(2002)03-0038-05
修稿时间:2002年6月4日

Genesis of Xuyaogou gold deposit in the southwest of Henan
CHANG Qiu-ling ,LU Xin-xiang ,XUE Qing.Genesis of Xuyaogou gold deposit in the southwest of Henan[J].Gold Geology,2002,8(3):38-42.
Authors:CHANG Qiu-ling  LU Xin-xiang  XUE Qing
Institution:CHANG Qiu-ling 1,LU Xin-xiang 1,XUE Qing 2
Abstract:The geological background, deposit character, ore controlling factors and deposit genesis were discussed. The fault, especially ductile shear belt controlled the mineralization mainly. The age of the mineralization and the granite was different and had the character of diachroneity and rerticality. Granite connected depth with shallow and caused deep auriferous metallogenetic fluid through rifted fractured zone uplifting and precipitation.
Keywords:gold deposit  metallogenetic fluid  metallogenetic mechanism  ductile shear belt  Henan
本文献已被 CNKI 维普 万方数据 等数据库收录!
设为首页 | 免责声明 | 关于勤云 | 加入收藏

Copyright©北京勤云科技发展有限公司  京ICP备09084417号