气候变化领域集成服务门户(CCPortal): Evidence for extreme partitioning of copper into a magmatic vapor phase

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DOI	10.1126/science.252.5011.1405
	Evidence for extreme partitioning of copper into a magmatic vapor phase
	Lowenstern J.B.; Mahood G.A.; Rivers M.L.; Sutton S.R.
发表日期	1991
ISSN	0036-8075
起始页码	1405
结束页码	1409
卷号	252 期号:5011
英文摘要	The discovery of copper sulfides in carbon dioxide- and chlorine-bearing bubbles in phenocryst-hosted melt inclusions shows that copper resides in a vapor phase in some shallow magma chambers. Copper is several hundred times more concentrated in magmatic vapor than in coexisting pantellerite melt. The volatile behavior of copper should be considered when modeling the volcanogenic contribution of metals to the atmosphere and may be important in the formation of copper porphyry ore deposits.
英文关键词	copper; emission; magmatic vapour; magmatic vapour phase; melt inclusion; metal; partitioning; vapour phase; volcano
语种	英语
来源期刊	Science
文献类型	期刊论文
条目标识符	http://gcip.llas.ac.cn/handle/2XKMVOVA/244581
作者单位	Department of Geology, Stanford University, Stanford, CA 94305; Department of Applied Science, Brookhaven National Laboratory, Upton, NY 11973
推荐引用方式 GB/T 7714	Lowenstern J.B.,Mahood G.A.,Rivers M.L.,et al. Evidence for extreme partitioning of copper into a magmatic vapor phase[J],1991,252(5011).
APA	Lowenstern J.B.,Mahood G.A.,Rivers M.L.,&Sutton S.R..(1991).Evidence for extreme partitioning of copper into a magmatic vapor phase.Science,252(5011).
MLA	Lowenstern J.B.,et al."Evidence for extreme partitioning of copper into a magmatic vapor phase".Science 252.5011(1991).