The trace element composition of scheelite from 19 well-documented reduced and oxidized
skarn systems was measured by laser ablation-inductively coupled plasma-mass …

Porphyry-skarn deposits are the major sources of Cu and Au in eastern China, and W is a
common byproduct of these mines. Scheelite is the W-bearing mineral in these deposits …

Skarn-type tungsten deposits are widely distributed all over the world and contribute more
than 70% of the world's W supply. The temporal relation between the W mineralization and …

The large-scale Yaogangxian W deposit, located in central of the Nanling metallogenic belt,
South China, comprises independent quartz vein-type and skarn-type W mineralization …

Huangshaping is a world-class skarn deposit hosting abundant W–Sn polymetallic
mineralization in the Nanling Range, South China. Although the geochemistry of skarn …

Geochemical gene is a new technique presented recently and its history is described and
classified into three stages up to the present. To construct a geochemical gene, five steps …

The Shizhuyuan oxidized skarn-greisen W–Sn deposit (South China) has widely developed
scheelite in the prograde skarn stage, retrograde skarn stage, oxide stage, sulfide-quartz …

Abstract The Xuefeng Uplift Belt (XUB), in the western part of the Jiannan Orogenic Belt
(JOB) South China, hosts numerous low-temperature W-Sb-Au deposits, including the Woxi …

Abstract The Xingjiashan W-Mo skarn deposit in the Jiaodong Peninsula, eastern China, is
hosted by the Paleoproterozoic metamorphic rocks and Mesozoic granitic stock. Four …

Scheelite is the main ore mineral in skarn-type tungsten (W-Mo, W-Sn, and W-Cu) deposits,
and is also a good proxy for ore-fluid evolution and mineralization. The Bastielieke deposit is …