REE geochemistry of lamprophyres in Baimazhai nickel deposit, Yunnan Province, China: implication for the mantle source region

Based on the REE geochemistry data from the Baimazhai nickel deposit, Yunnan Province,the authors modeled the composition of the mantle source region by way of petrological mixing calculation,and further discussed the genesis of this type of rocks. Both element geochemistry data and mixing calculati...

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Veröffentlicht in:Acta geochimica 2005-07, Vol.24 (3), p.273-279
1. Verfasser: 管涛 黄智龙 许成 张振亮 严再飞 申宝剑
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description Based on the REE geochemistry data from the Baimazhai nickel deposit, Yunnan Province,the authors modeled the composition of the mantle source region by way of petrological mixing calculation,and further discussed the genesis of this type of rocks. Both element geochemistry data and mixing calculation showed that lamprophyres in the Baimazhai nickel deposit were derived from a metasomatism-enrichment mantle and the fluids resulted from dehydration of a subducted slab which is comprised of ALK-,LREE-and incompatible element-rich sediments.
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ispartof Acta geochimica, 2005-07, Vol.24 (3), p.273-279
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1993-0364
2365-7499
language eng
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source Alma/SFX Local Collection; SpringerLink Journals - AutoHoldings
subjects Dehydration
Fluids
Geochemistry
Nickel
Petrology
Sediments
Volcanoes
地球化学
沉积作用
煌斑岩
title REE geochemistry of lamprophyres in Baimazhai nickel deposit, Yunnan Province, China: implication for the mantle source region
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