Supported by the National Natural Science Foundation of China(41702110);China National Science and Technology Major Project(2017ZX05001-001);National Key Research and Development Project(2017YFC0601405).
Based on comprehensive analysis of typical outcrops, latest deep wells drilled and high resolution seismic profiles in the study area, we examined the geologic structure of the Kelameili range, and analyzed the struct...
This research was jointly granted by the Key Scientific Research Project of Inner Mongolia Geological Survey(2004-05);the National Natural Science Foundation of China(Grant No.40272088).
The Dajing Cu-Sn-polymetallic ore deposit is famous for its large scale, abundant associated elements, narrow and closely-spaced development of ore veins and high grade, but exploration within the mining district and ...
The LA-ICP-MS analyses were carfled out at the laboratory of Prof.GUnther at Institute of Science and Technology,Switzerland.Dr.Yuan Honglin is thanked for assistance during the analyses.Profs.Ni Pei and Fan Hongrui are thanked for constructive comments.The work was supported by National Natural Science Foundation of China(Grant No.40273021);National 973 Project(Grant No.2001CB409806).
从 Dajing 存款的 Sn-Cu 矿石身体并且从 Huanggangliang 存款的 Sn 矿石身体在荧石和石英套住的单个液体包括上的 LA-ICP-MS 分析被进行用液体的 Rb/Sr 和 Sn/Cu 比率在 Dajing 存款跟踪 Cu 富有、 Sn 富有的液体的来源和进化。在 theD...
the Knowledge Innovation Program of the Chinese Academy of Sciences (Grant No.KZCX1-07); the National Natural Science Foundation of China(Grant No.40273021); 973 National Project (Grant No.2001cb409806).
Fluid inclusions from the Dajing and Caijiaying deposits have nearly the same homogenization temperature. Correlation between temperature and salinity shows that both Sn- and Cu-bearing fluids Sn and Cu were present i...
This work was supported by the Chinese Academy of Sciences(Grant Nos.KZCX1-07-04 and IGG CX2000-02).
Dajing Cu-Sn-Ag-Pb-Zn ore deposit, in the Inner Mongolia Autonomous Region of China, is a fissure-filling hydrothermal ore deposit. The d D values of quartz-hosted inclusion water are centered at -100 — -130. The d 3...
This work was supported by the Chinese Academy of Sciences (Grant Nos. KZCX2-104 and KZ951-A1-401);the Ministry of Science and Technology of China (pre-selected 39 project).
By comparing PGE patterns of sulfide ores with that of basic-ultrabasic dikes occurring in the Dajing Cu-polymetallic deposit, we discover that there are similar positive slopes between the basic-ultrabasic dikes and ...