摘要
槐树庄金矿位于华北板块南缘与秦岭造山带接合部位,其成矿作用与构造和热液有关。通过对其矿床地质特征、同位素地质特征、成矿温度及矿床成因等方面的研究,认为其成矿物质来源为熊耳群火山岩,成因类型属于中低温构造蚀变岩型金矿床。
Hushuzhuang Au deposit lies in junction place of North China Plate South border and Qinling orogenic belt,which is mainly related to tectonic and hydrothermal activity. Studies on geology,isotopes, ore-forming temperature and metallogenesis indicate that the ore-forming material derived from volcanic rock of xiong' er group. The deposit belongs to Au deposit related to low-to-moderate temperature tectonic altered rock.
出处
《矿产与地质》
2004年第1期18-21,共4页
Mineral Resources and Geology
关键词
金矿床
矿床成因
地质特征
河南省槐树庄
Huaishuzhuang
Au deposit
geological characteristics
deposit genesis
henan provice
