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川陕甘地区卡林型金矿对比研究
引用本文:喻光明,郭华.川陕甘地区卡林型金矿对比研究[J].四川地质学报,2010,30(2):163-169.
作者姓名:喻光明  郭华
作者单位:中国人民武装警察部队黄金第十二支队,成都,610036
摘    要:我国卡林型金矿床主要分布于扬子陆块西南缘的板内古生代一中生代沉降带和西北缘古生代一中生代造山带。川陕甘地区是我国著名的“金三角”地区,该区成矿条件好,金矿床(点)分布密集,成因类型多,规模大,是国内具有大型和超大型金矿成矿条件的成矿远景区。对比区内的典型矿床,总结成矿规律,对指导该区面上找矿具有一定的现实意义。

关 键 词:卡林型金矿  对比  川陕甘地区

Comparison of Geological and Geochemical Features of Carlin-type Au Deposits in the Sichuan Shaanxi-Gansu Border Region
YU Guangming,GUO Hua.Comparison of Geological and Geochemical Features of Carlin-type Au Deposits in the Sichuan Shaanxi-Gansu Border Region[J].Acta Geologica Sichuan,2010,30(2):163-169.
Authors:YU Guangming  GUO Hua
Institution:(Gold Geological Party No.12, CAPF, Chengdu 610036)
Abstract:Carlin-type Au deposits in China occur in Paleozoic-Mesozoic depression zone in southwest marginal region and Paleozoic-Mesozoic orogenic zone in northwest marginal region of the Yangtze landmass The Sichuan-Shaanxi-Gansu border region is the famous Au delta in China where there are favorable ore-forming condition and many Au ore occurrences. This paper deals with typical deposits and metallogenic law in this region.
Keywords:Au deposit  comparison  Sichuan-Shaanxi-Gansu border region
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