supported by grants from the National Key R&D Program of China(2016YFC0600207);the Chinese 973 project(2012CB416804);the National Natural Science Foundation of China(41503039);the ‘‘CAS Hundred Talents’’Project to J.F.Gao(Y5CJ038000)
The Xinqiao deposit is one of several polymetallic deposits in the Tongling ore district. There are two types of mineralization in the Xinqiao: skarn-type and stratiform-type. The skarn-type mineralization is charact...
financially supported by the National Basic Research Program of China (No. 2015CB452605);the Natural Science Foundation of China (No. 41602089);Fundamental Research Funds for the Central Universities (No. 20170713174019)
The newly-discovered Donglufang Moe Cu porphyry-skarn deposit is located in the southern Yidun Terrane, southeast Tibet, with more than 80 million tonnes(Mt) of reserves(grading 0.15 wt.% Mo and0.48 wt.% Cu) hosted in...
supported by the National Basic Research Program of China(973 Program:2012CB416802);the National Special Research Programs for Non-Profit Trades(Sponsored by MLR,201311136);the Basic Scientific Research Operation Cost of StateLeveled Public Welfare Scientific Research Courtyard (K1203)
The Chengchao iron deposit,the largest high-grade skarn iron deposit in southeastern Hubei Province,contains considerable amounts of magnetite and by-product anhydrite.To obtain better understanding of the ore-formati...
supported by the National Natural Science Foundation of China(Grant Nos:49625304 and 49633120);the Ministry of Land and Resources of China(Grant No.2000401);the Ministry of Science and Technology of China through a National Climbing Project 95-P-39.
REE and other trace elements in the altered marbles, massive skarns and ores, as well as garnet and quartz were determined in order to examine the behaviors of trace elements during hydrothermal alteration. It is demo...