闽西南地区大地构造演化和矿床时空分布规律

张振杰, 左仁广. 闽西南地区大地构造演化和矿床时空分布规律[J]. 岩石学报, 2015, 31(1): 217-229.
引用本文: 张振杰, 左仁广. 闽西南地区大地构造演化和矿床时空分布规律[J]. 岩石学报, 2015, 31(1): 217-229.
ZHANG ZhenJie, ZUO RenGuang. Tectonic Evolution of southwestern Fujian Province and spatial-temporal distribution regularity of mineral deposits[J]. Acta Petrologica Sinica, 2015, 31(1): 217-229.
Citation: ZHANG ZhenJie, ZUO RenGuang. Tectonic Evolution of southwestern Fujian Province and spatial-temporal distribution regularity of mineral deposits[J]. Acta Petrologica Sinica, 2015, 31(1): 217-229.

闽西南地区大地构造演化和矿床时空分布规律

  • 基金项目:

    本文受国家自然科学基金项目(41372007)和教育部新世纪优秀人才支持计划(NCET-13-1016)联合资助.

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Tectonic Evolution of southwestern Fujian Province and spatial-temporal distribution regularity of mineral deposits

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  • 在充分吸收前人工作成果的基础上,讨论了闽西南地区的主要矿床类型及其特征,将闽西南地区的矿床划分为三个矿床成矿系列:晋宁期与海相火山作用有关的铅、锌、银多金属块状硫化物矿床成矿系列;海西-印支期与火成岩有关的铁、铜、铅、锌多金属矿床成矿系列;燕山期与中酸性火成岩有关的铁、铜、铅、锌、钼、钨、锡、金、银、铀等多金属矿床成矿系列。其中,与燕山期有关的矿床成矿系列可进一步划分为侏罗纪早期与壳幔混合源I型花岗闪长岩有关的铁、铜、铅、锌矿床成矿亚系列;侏罗纪晚期与壳源S型花岗质岩体有关的钨、锡、钼、铋多金属矿床成矿亚系列;早白垩世与壳源型中酸性侵入岩有关的层控矽卡岩型铁、铜、铅、锌、钼多金属矿床成矿亚系列;早白垩世与壳幔混合源型中酸性侵入岩-次火山作用有关的金、银、铜、钼、铅、锌、铀等多金属矿床成矿亚系列。总结研究提出了各成矿(亚)系列的形成背景、时空分布规律,初步认为晋宁期VMS型多金属矿床形成于华南联合陆块拉张裂解形成的政和-大埔海底双峰式火山盆地环境,海西-印支期岩浆热液-斑岩型金属矿床形成于陆内伸展与挤压环境交替出现的岩浆侵入过程中,而燕山期成矿(亚)系列则形成于太平洋构造域时期的陆内伸展与挤压环境交替出现的岩浆侵入与火山喷发的过程中。
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收稿日期:  2014-01-01
修回日期:  2014-10-07
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