ISSN 1009-6248CN 61-1149/P 双月刊

主管单位:中国地质调查局

主办单位:中国地质调查局西安地质调查中心
中国地质学会

    高级检索
    陈国忠, 龚全胜, 梁志录, 张愿宁, 麻红顺. 西秦岭甘肃段特大型金矿床的地质地球化学特征及其成岩成矿年龄[J]. 西北地质,2017,50(4): 91-104.
    引用本文: 陈国忠, 龚全胜, 梁志录, 张愿宁, 麻红顺. 西秦岭甘肃段特大型金矿床的地质地球化学特征及其成岩成矿年龄[J]. 西北地质,2017,50(4): 91-104.
    CHEN Guozhong, GONG Quansheng, LIANG Zhilu, ZHANG Yuanning, MA Hongshun. Geological, Geochemical Characteristics and Diagenetic Age of the Super-large Gold Deposits in Western Qinling, Gansu Province[J]. Northwestern Geology,2017,50(4): 91-104.
    Citation: CHEN Guozhong, GONG Quansheng, LIANG Zhilu, ZHANG Yuanning, MA Hongshun. Geological, Geochemical Characteristics and Diagenetic Age of the Super-large Gold Deposits in Western Qinling, Gansu Province[J]. Northwestern Geology,2017,50(4): 91-104.

    西秦岭甘肃段特大型金矿床的地质地球化学特征及其成岩成矿年龄

    Geological, Geochemical Characteristics and Diagenetic Age of the Super-large Gold Deposits in Western Qinling, Gansu Province

    • 摘要: 西秦岭是中国具有大型、特大型金矿成矿条件的成矿带,通过对西秦岭甘肃段4个特大型金矿之间及其卡林型金矿、造山型金矿的地质、地球化学特征对比研究表明:这4个特大型金矿均具有多期多次成矿的特点,且具有由卡林型金矿向造山型金矿过渡的特征,成矿作用发生在碰撞造山阶段的挤压向伸展转换期,代表了一种新的成矿类型,建议定义为"卡林-造山复合型",特大型金矿成矿时间为127~216 Ma,成矿背景及成矿时间具有偏在性。

       

      Abstract: The West Qinling metallogenic belt has good condition for forming large and super-large gold deposits in China. In this paper, the geological and geochemical characteristics of four super-large deposits in West Qinling, Gansu Province have been analyzed, and they are compared with the ones of Karlin-type and orogenic gold deposits. The results show that these four super-large gold deposits have many characteristics of multi-stage mineralization, and they have the transition characteristics of changing from Karlin-type gold deposit to orogenic gold deposit.The gold mineralization was occurred in the collision orogenic stage, which has been defined as "Carlin-orogenic compound type".The metallogenic age of these super-large gold deposits is 127~216 Ma, the metallogenic background and time show the metallogenic preferentiality.

       

    /

    返回文章
    返回