Redistribution of Trace Elements During Shock-inducd Melting and Phase Tranzition of Minerals in the

来源 :11th International Congress of Applied Mineralogy,11thICAM(第 | 被引量 : 0次 | 上传用户：regelus

【摘要】

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【作者】

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XIE Xiande ZHANG Hong WANG Chunyun

【机构】

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Key Laboratory of Mineralogy and Metallogeny, Guangzhou Institute of Geochemistry,Chinese Academy of

【出处】

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11th International Congress of Applied Mineralogy,11thICAM(第

【发表日期】

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2013年4期

【关键词】

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trace element shock melting phase transition LA-ICP-MS Suizhou meteorite

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The Suizhou meteorite is an L6 chondrite.This meteorite is consisted of olivine, low-Ca pyroxene,plagioclase, FeNi metal, troilite, whitlockite, chlorapatite, chromite and ilmenite.Olivine and pyroxene grains display shock-induced mosaic texture, and most plagioclase grains were melted and transformed to maskelynite.This meteorite contains a few very thin shock-produced melt veins ranging from 20 to 100 μm in width.

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Redistribution of Trace Elements During Shock-inducd Melting and Phase Tranzition of Minerals in the

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