Article ID | Journal | Published Year | Pages | File Type |
---|---|---|---|---|
4731868 | Journal of Asian Earth Sciences | 2011 | 12 Pages |
Abstract
⺠Nephrite forms through: dolomitic marble â tremolite or diopside â tremolite. ⺠Alamas deposit shows nephrite color zones with increasing contents of Cr and TFe2O3. ⺠Fluid inclusions in tremolite indicate nephrite formed above 293 °C. ⺠Ore-forming fluids for nephrite have meteoric, magmatic water and CO2 from dolomite. ⺠Metasomatic and dolomite-related origin is suggested for Alamas nephrite deposit.
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Authors
Yan Liu, Jun Deng, Guanghai Shi, Tzen-Fu Yui, Guibin Zhang, Maituohuti Abuduwayiti, Liqiang Yang, Xiang Sun,