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硬玉成矿理论综述

黄文清

安徽地质Issue(4):278-280,3.
安徽地质Issue(4):278-280,3.

硬玉成矿理论综述

A discussion on jadeite formation mechanism

黄文清1

作者信息

  • 1. 国家金银制品质量监督检验中心南京,江苏 南京 210028
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摘要

Abstract

  As a rare gemstone resource, jadeite has seen a rapid rise in price in recent years, resulting in warming study on jadeite formation mechanism. This paper summarized geological features of the jadeite deposits in Burma, the major production area of gemstone-grade jadeite, introduced four theories on jadeite formation such as magmatic origin, meta-morphic origin, double-metasomatic origin and metasomatic origin, and thought it more scientifically reasonable that jadeite had been directly crystallized from silicate melt under high-T and high-P conditions. Based on its texture, inclu-sion, mineral assemblage and T-P conditions at formation, jadeitite was thought to have been formed from magma by crystallization at the lower pressure limit of P>1.5GPa and temperature range of 650 to 800℃. This paper discussed the source of the melt and argued that the silicate melt might have been related to diagenesis and metallogenesis of meta-morphic anatexis.

关键词

硬玉/成矿理论/熔体/变质深熔/综述

Key words

jadeite/metallogenic theory/melt/metamorphic anatexis/summarization

分类

天文与地球科学

引用本文复制引用

黄文清..硬玉成矿理论综述[J].安徽地质,2012,(4):278-280,3.

安徽地质

1005-6157

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