GIG OpenIR  > 中科院广州地化所(2009-)  > 会议论文
橄榄岩水饱和固相线及第二临界端点研究:微量元素限制
王锦团; 熊小林; Eiichi Takahashi
Source Publication第八届全国成矿理论与找矿方法学术讨论会论文摘要文集
2017-12-09
Conference Date2017-12-09
Conference Place中国江西南昌
Country中国
Indexed By其他
Language中文
Keyword橄榄岩 固相线 水饱和 微量元素含量
Abstract橄榄岩是上地幔的主要组成部分,是玄武质岩浆的源岩。准确限定橄榄岩固相线是认识玄武质岩浆成因的关键。俯冲带水饱和条件下橄榄岩固相线研究是理解岛弧岩浆成因,探究俯冲带富水流体与含水熔体及超临界流体形成条件,限定俯冲带水的运移能力的基础。然而,受限于高温高压条件实验中富水流体与含水熔体在淬火过程中难以保存,对于淬火产物的不同解释导致橄榄岩水饱和固相线及超临界流体的形成
Document Type会议论文
Identifierhttp://ir.gig.ac.cn/handle/344008/35535
Collection中科院广州地化所(2009-)_会议论文
Recommended Citation
GB/T 7714
王锦团,熊小林,Eiichi Takahashi. 橄榄岩水饱和固相线及第二临界端点研究:微量元素限制[C],2017.
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C2017_王锦团.pdf(971KB)会议论文 暂不开放CC BY-NC-SAApplication Full Text
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