安徽西冲钼矿床细粒花岗岩的岩石定年、岩石化学及与成矿的关系研究

谢玉玲, 李腊梅, 郭翔, MEFFRESebastien, CHANGZhaoShan, 张健, 姚羽, 王爱国. 安徽西冲钼矿床细粒花岗岩的岩石定年、岩石化学及与成矿的关系研究[J]. 岩石学报, 2015, 31(7): 1929-1942.
引用本文: 谢玉玲, 李腊梅, 郭翔, MEFFRESebastien, CHANGZhaoShan, 张健, 姚羽, 王爱国. 安徽西冲钼矿床细粒花岗岩的岩石定年、岩石化学及与成矿的关系研究[J]. 岩石学报, 2015, 31(7): 1929-1942.
XIE YuLing, LI LaMei, GUO Xiang, MEFFRE Sebastien, CHANG ZhaoShan, ZHANG Jian, YAO Yu, WANG AiGuo. Chronology, petrochemistry of fine grained granite and their implication to Mo-Cu mineralization in Xichong Mo deposit, Anhui Province, China.[J]. Acta Petrologica Sinica, 2015, 31(7): 1929-1942.
Citation: XIE YuLing, LI LaMei, GUO Xiang, MEFFRE Sebastien, CHANG ZhaoShan, ZHANG Jian, YAO Yu, WANG AiGuo. Chronology, petrochemistry of fine grained granite and their implication to Mo-Cu mineralization in Xichong Mo deposit, Anhui Province, China.[J]. Acta Petrologica Sinica, 2015, 31(7): 1929-1942.

安徽西冲钼矿床细粒花岗岩的岩石定年、岩石化学及与成矿的关系研究

  • 基金项目:

    本文受国土资源部公益性行业基金项目(201011011)和中国地质调查局项目(2014-01-020-010)联合资助.

Chronology, petrochemistry of fine grained granite and their implication to Mo-Cu mineralization in Xichong Mo deposit, Anhui Province, China.

  • 西冲钼矿是大别成矿带东段近年新发现的斑岩型钼-多金属矿床,其矿床学和矿床地球化学研究少见报导。该研究成果丰富了我国斑岩-矽卡岩型钼钨-多金属矿床研究成果,同时对指导区域找矿具有一定意义。本文在详细的野外地质调研基础上,对大别成矿带西冲钼矿区出露的主要岩石单元、矿化和蚀变特征、细粒花岗岩的岩石学、岩石化学和成岩年代学进行了系统的研究。结果表明,矿区出露的主要侵入岩单元由老至新依次为:石英二长岩、细粒花岗岩(130.8±1.1Ma)及双峰式脉岩组合(131.9±1.4Ma和131.3±1.6Ma),其均为燕山期岩浆活动产物,产于华北与扬子陆块拼合后的陆内环境。矿化类型以脉状、网脉状和浸染状为主,为一斑岩型钼-多金属矿床。矿区蚀变发育,包括黑云母-磁铁矿化、钾长石化、硅化、石英-绢云母化、石英-绿帘石化、绿泥石-碳酸盐化和泥化,且空间上具有一定的分带规律。矿区已知矿化、蚀变及Cu-Mo化探异常的空间展布与细粒花岗岩关系密切,且细粒花岗岩中具有高的Mo含量,表明该矿床的形成主要与细粒花岗岩有关。岩石化学结果表明,细粒花岗岩属过铝质-准铝质、高钾钙碱性-钾玄质过渡岩石,锆石U-Pb年龄与双峰式脉岩的在误差范围内一致,表明其均形成于大别造山带大规模伸展背景。
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出版历程
收稿日期:  2014-07-10
修回日期:  2015-03-16
刊出日期:  2015-07-31

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