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Tungsten mineralization process and oxygen fugacity evolution in the Weijia W deposit, South China: Constraints from the microstructures, geochemistry, and oxygen isotopes of scheelite, garnet, and calcite
点击次数：
影响因子：3.714
DOI码：10.1016/j.oregeorev.2022.104952
所属单位：地信院
教研室：地质资源系
发表刊物：Ore Geological Reviews
刊物所在地：NETHERLAND
项目来源：深地研发2018YFC0603901
论文类型：文章
论文编号：104952
学科门类：理学
一级学科：地质学
卷号：146
是否译文：否
发表时间：2022-05-22
收录刊物：SCI
发布期刊链接：https://doi.org/10.1016/j.oregeorev.2022.104952
附件：
上一条：Geochronology, Whole-Rock Geochemistry, and Sr-Nd-Hf Isotopes of Granitoids in the Tongshanling Ore Field, South China: Insights into Cu and W Metallogenic Specificity
下一条：Origin and evolution of W mineralization in the Tongshanling Cu–polymetallic ore field, South China: Constraints from scheelite microstructure, geochemistry, and Nd–O isotope evidence