长江中下游成矿带成岩成矿作用研究进展

周涛发,范裕,袁峰. 长江中下游成矿带成岩成矿作用研究进展[J]. 岩石学报, 2008, 24(8).
引用本文: 周涛发,范裕,袁峰. 长江中下游成矿带成岩成矿作用研究进展[J]. 岩石学报, 2008, 24(8).
ZHOU TaoFa,FAN Yu,YUAN Feng. Advances on petrogensis and metallogeny study of the mineralization belt of the Middle and Lower Reaches of the Yangtze River area[J]. Acta Petrologica Sinica, 2008, 24(8).
Citation: ZHOU TaoFa,FAN Yu,YUAN Feng. Advances on petrogensis and metallogeny study of the mineralization belt of the Middle and Lower Reaches of the Yangtze River area[J]. Acta Petrologica Sinica, 2008, 24(8).

长江中下游成矿带成岩成矿作用研究进展

  • 基金项目:

    国家自然科学基金,国家重点基础研究发展计划(973计划),教育部高等学校博士学科点专项科研基金,安徽省地质勘查专项费项目,安徽省优秀青年科技基金

Advances on petrogensis and metallogeny study of the mineralization belt of the Middle and Lower Reaches of the Yangtze River area

  • 长江中下游成矿带是中国最主要的铜铁金多金属成矿带之一,由鄂东南、九瑞、安庆一贵池、铜陵、庐枞和宁芜等位于断隆区、断凹区和隆凹过渡区的多个矿集区组成,成矿带形成经历了中生代转换复合的构造体制、强烈的壳幔相互作用等复杂的大陆动力学过程,具有爆发式的多阶段岩浆活动、大规模的铜铁金多金属成矿作用和多类型的复杂成矿系统演化,以及深部找矿潜力巨大等特点,是开展陆内动力学过程与成岩成矿作用研究的不可多得的天然实验室.本文从成岩成矿构造背景、地球动力学过程、时空格架以及成矿流体系统演化等方面,对近十年来国内外学者对该成矿带成岩成矿作用研究的主要成果和进展作一初步归纳,并简要分析了下一步研究的主要科学问题.
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刊出日期:  2008-08-31

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