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甘肃西秦岭金矿富集区花岗岩与金成矿作用的关系
引用本文:殷勇,赵彦庆.甘肃西秦岭金矿富集区花岗岩与金成矿作用的关系[J].甘肃地质学报,2006,15(1):36-41.
作者姓名:殷勇  赵彦庆
作者单位:甘肃地矿科技信息中心 甘肃兰州730000(殷勇),甘肃省地质调查院 甘肃兰州730000(赵彦庆)
摘    要:依据甘肃西秦岭金矿富集区矿床和相关花岗岩的同位素年龄和稳定同位素数据,探讨了该区金矿床成矿作用与花岗岩成岩作用的关系及成矿物质来源。从数据显示,成岩和成矿作用均发生在侏罗纪;成岩年龄集中分布在200Ma~171Ma;大规模成矿作用年龄分布在195Ma~140Ma;成矿事件同步或略滞后于花岗岩浆活动;相关花岗岩是地壳物质重熔而成的S型;花岗岩浆侵入是该区金矿形成的主导因素;成矿物质和流体来源于地壳。

关 键 词:甘肃西秦岭  金矿富集区  花岗岩  同位素年龄  稳定同位素
文章编号:1004-4116(2005)01-0036-0006
收稿时间:2006-03-08

RELATIONGSHIP BETWEEN GRANITE AND GOLD MINERALLZATION IN THE GOLD ENRICHMENT AREA OF WESTERN QINLING, GANSU PROVINCE
YIN Yong and ZHAO Yan-qing.RELATIONGSHIP BETWEEN GRANITE AND GOLD MINERALLZATION IN THE GOLD ENRICHMENT AREA OF WESTERN QINLING, GANSU PROVINCE[J].Acta Geologica Gansu,2006,15(1):36-41.
Authors:YIN Yong and ZHAO Yan-qing
Institution:1. Gansu Geology and Mineral Resouces Information Center, Lanzhou 730000, China ; 2. Geological Survey of Gansu Province, Lanzhou 730000, China
Abstract:The data of isotopic age and stable isotope for deposit and related granitic in the gold enrichment area of western Qinling of Gansu Province were collected, and the relationship between gold mineralization and diagenesis, and metallogenetic material source in this area was discussed. The statistics show that both mineral- ization and diagenesis occurred in Jurassic, diagenetic age is distributed in 220Ma- 171Ma, most in 200Ma- 171Ma; and big scale mineralization occurred in 195Ma-140Ma. Metallogenic event occurred in same time or a little late with granitic magmatic activity. Metallogenic material and fluid were from earth - crust, related granite is S- type ganitic magma that formed by crustal material remelting, and its and its intrusion is master factor which led to form gold deposit in this area.
Keywords:Western Qinling  Gansu Province  Gold enrichment area  Granite  Isotopic age  Stable isotope
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