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峨眉山玄武岩的输送通道:云南元谋朱布岩体
朱丹; 徐义刚; 罗泰义; 宋谢炎; 陶琰; 黄智龙; 朱成明; 蔡恩照
2007
Source Publication矿物学报
Volume27Issue:3Pages:273-280
metadata_24其它
Abstract朱布镁铁-超镁铁侵入岩赋存有中型硫化物铂族元素矿床。根据岩体大小和矿床储量的简单质量平衡计算,矿床的形成需要至少3000倍现存岩体体积的岩浆参与成矿,因此朱布岩体应该是峨眉山玄武岩的输送通道。岩体的年龄、地质特征、地球化学都支持这个结论。岩体的原始岩浆应该属于峨眉山高钛玄武岩.
Keyword镁铁-超镁铁岩
Subject Area中国典型特殊区带大规模成矿作用及其动力学
Funding Organization国家重点基础研究发展计划(编号:2007CB411401);国家自然科学基金(批准号:40572054;40274027;40573020)
Indexed ByCSCD
Language中文
CSCD IDCSCD:3057087
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Document Type期刊论文
Identifierhttp://ir.gyig.ac.cn/handle/352002/498
Collection矿床地球化学国家重点实验室_矿床地球化学国家重点实验室_期刊论文
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GB/T 7714
朱丹,徐义刚,罗泰义,等. 峨眉山玄武岩的输送通道:云南元谋朱布岩体[J]. 矿物学报,2007,27(3):273-280.
APA 朱丹.,徐义刚.,罗泰义.,宋谢炎.,陶琰.,...&蔡恩照.(2007).峨眉山玄武岩的输送通道:云南元谋朱布岩体.矿物学报,27(3),273-280.
MLA 朱丹,et al."峨眉山玄武岩的输送通道:云南元谋朱布岩体".矿物学报 27.3(2007):273-280.
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