古生代镁铁、超镁铁岩浆矿床成矿系列与成矿作用
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引用本文:.2004.Metallogenic Series and Ore-forming Processes of Mafic-Ultramafic Magmatic Deposits in Paleozoic Era[J].Mineral Deposits,23(Z):131~136
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Author NameAffiliation
汤中立,钱壮志,闫海卿,焦建刚 长安大学 
基金项目:中国工程院咨询项目(6/2001c)和地质大调查综合研究项目(K1.4-3-2)和(200110200058)
中文摘要:岩浆矿床一直受到人们的关注,文章在对古生代22个岩浆矿床成矿系列及23个矿床式进行总结的基础上,划分了中国古生代岩浆矿床类型,归纳出岩浆矿床的3种成矿方式:① 岩浆侵入体成矿;② 与大陆溢流玄武岩有关的成矿;③与蛇绿岩有关的成矿。对Fe-V-Ti的大规模成矿作用进行了总结。通过上述研究和总结,提出了古生代岩浆矿床的勘查方向及存在的问题。
中文关键词:古生代  岩浆矿床  成矿系列  成矿作用
 
Metallogenic Series and Ore-forming Processes of Mafic-Ultramafic Magmatic Deposits in Paleozoic Era
Abstract:Much importance has always been attached to magmatic deposits. Based on a summarization of twenty-two Paleozoic metallogenic series of magmatic deposits and twenty-three ore deposit models, this paper has classified types of Paleozoic magmatic deposits in China, and generalized three kinds of metallogenic patterns for magmatic deposits. They are (1) mineralization of magmatic intrusion, (2) mineralization associated with continental flood basalt; (3) mineralization related to ophiolites. The large-scale Fe-V-Ti mineralization is also summarized. The prospecting directions and existing problems related to Paleozoic magmatic deposits are also discussed in this paper.
keywords:Paleozoic, magmatic deposit, metallogenic series, metallogenesis
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