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作 者:ZHAOLei HAOJinhua DINGYifei LIUYulong
机构地区:[1]ChinaUniversity,ofGeosciences(Beijing),Beijing100083
出 处:《Acta Geologica Sinica(English Edition)》2004年第1期118-120,共3页地质学报(英文版)
基 金:the National Natural Foundation of China grants 40273016 , 49973013
摘 要:Based on studies of petrography, mineralogy and mineral chemistry, deep mantle fluids and their products in kimberlites and diamonds can be assorted into the ultradeep fluid-transmitted minerals with an oxygen-free feature, the deep fluid metasomatized-minerals characterized by enrichment in TiO2, K2O, BaO, REE and Fe3+, and the deep fluid-reformed minerals. The three types show a successive descent in fluid origin depth and metasomatism strength, and they have brought forth a series of corresponding metasomatic products.Based on studies of petrography, mineralogy and mineral chemistry, deep mantle fluids and their products in kimberlites and diamonds can be assorted into the ultradeep fluid-transmitted minerals with an oxygen-free feature, the deep fluid metasomatized-minerals characterized by enrichment in TiO2, K2O, BaO, REE and Fe3+, and the deep fluid-reformed minerals. The three types show a successive descent in fluid origin depth and metasomatism strength, and they have brought forth a series of corresponding metasomatic products.
关 键 词:KIMBERLITE DIAMOND assortment of deep mantle fluids PRODUCTS
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