Match!
Zhaochong Zhang
China University of Geosciences
GeologyGeochemistryMagmaZirconPetrology
101Publications
28H-index
2,137Citations
What is this?
Publications 116
Newest
#1Zhiguo Cheng (China University of Geosciences)H-Index: 8
#2Zhaochong Zhang (China University of Geosciences)H-Index: 28
Last. M. Santosh (University of Adelaide)H-Index: 85
view all 9 authors...
Source
#1Meng Wang (China University of Geosciences)H-Index: 5
#2Jun Deng (China University of Geosciences)H-Index: 33
Last. Francois Holtz (Leibniz University of Hanover)H-Index: 50
view all 10 authors...
The solubility of scheelite in evolved granitic magmas (Qz-Ab-Or-An system with minor FeOtotal, TiO2, and CaO added) was studied experimentally at 200 MPa, 750–850 °C and relatively oxidizing condition (logfO2 = NNO + 2.3, where NNO is Ni-NiO oxygen buffer). Water-saturated granitic melts have been equilibrated with seeds of scheelite crystals. The resulted WO3 contents in the melts vary only slightly from 0.21 to 0.32 wt.% WO3 over the investigated temperature and compositional range (0.7 to 1....
Source
#1Jiang Zhu (China University of Geosciences)H-Index: 3
#2Zhaochong Zhang (China University of Geosciences)H-Index: 28
Last. Ziliang Jin (China University of Geosciences)H-Index: 3
view all 4 authors...
Abstract Carlin-style gold deposits constitute one of the most important types of Au resources in the world. Previous studies on these deposits correlated the source of Au with metal-enriched sedimentary formations or metasomatized subcontinental lithospheric mantle (SCLM) associated with oceanic subduction. The role of mantle plumes in generating Carlin-style deposits has remained enigmatic due to lack of adequate evidence. Here we investigate the second largest Carlin-style Au province in the ...
Source
#1Abulimiti Aibai (PKU: Peking University)H-Index: 1
#2Zhaochong Zhang (China University of Geosciences)H-Index: 28
Last. M. Santosh (University of Adelaide)H-Index: 85
view all 5 authors...
Abstract The East Junggar region links the Kazakhstan-Junggar plate with the Siberian Craton along the western part of the Central Asian Orogenic Belt. Among the major ore deposits in this region, the Xilekuduke molybdenite deposit is a unique example of Mo-dominated porphyry. Molybdenum and copper mineralization here occur as disseminated sulfides or veinlets mainly in granite porphyry and monzogranite, with a prominent alteration from an inner potassic, through sericitic to an outer propylitic...
1 CitationsSource
#1Fengmei Chai (XJU: Xinjiang University)H-Index: 11
#2Zhaochong Zhang (China University of Geosciences)H-Index: 28
Last. Qiangfen XuH-Index: 1
view all 7 authors...
Abstract The Tianshan in China forms the southern part of the Central Asian Orogenic Belt (CAOB) and also hosts important polymetallic resources. Here we investigate the Huangtupo medium–size copper–zinc deposit, located in the central part of the Kalatag copper Polymetallic Belt with a view to evaluate the nature and genesis of the early Paleozoic volcanogenic massive sulfide (VMS) Cu—Zn deposits. This deposit is correlated to intermediate–felsic volcano–sedimentary sequences of the early Paleo...
Source
#1Xianghui Fei (China University of Geosciences)H-Index: 2
#2Zhaochong Zhang (China University of Geosciences)H-Index: 28
Last. M. Santosh (University of Adelaide)H-Index: 85
view all 4 authors...
Source
#1Hongbo Li (China University of Geosciences)H-Index: 4
#2Zhaochong Zhang (China University of Geosciences)H-Index: 28
Last. Ronghao Pan (China University of Geosciences)H-Index: 1
view all 7 authors...
Abstract The Neoproterozoic magmatic suites in South China have been central to the debate over the assembly and disruption of the Rodinia supercontinent. In this study, we report LA-ICP-MS zircon U-Pb ages, as well as mineralogical, geochemical and Sr-Nd isotopic data on the Mid-Neoproterozoic mafic dykes in the Xichang area along the western margin of the Yangtze Block. The zircon U-Pb data yield ages in the range of 795–743 Ma. Based on available age data, the magmatism along the western marg...
Source
#1Jie MengH-Index: 1
#2Hou-Min LiH-Index: 8
Last. Zhe SongH-Index: 1
view all 6 authors...
The origin of the Zhaoanzhuang serpentine-magnetite deposit in the southern North China Craton (NCC) is highly disputed, with some investigators having proposed an ultramafic origin, whereas others favor a chemical sedimentary origin. These discrepancies are largely due to the difficulty in determining the protolithic characteristics of the highly metamorphosed rocks. Sulfur, magnesium, and boron isotope geochemistry combined with detailed petrography was carried out in this study to constrain t...
Source
#1Qiuhong Xie (China University of Geosciences)H-Index: 4
#2Zhaochong Zhang (China University of Geosciences)H-Index: 28
Last. Xianghui Fei (China University of Geosciences)H-Index: 2
view all 7 authors...
1 CitationsSource
#1Weiliang Kong (China University of Geosciences)H-Index: 1
#2Zhaochong Zhang (China University of Geosciences)H-Index: 28
Last. M. Santosh (University of Adelaide)H-Index: 85
view all 5 authors...
Abstract The South Tianshan Orogenic Belt (STOB) occupies the southwestern margin of the Central Asian Orogenic Belt (CAOB), and is the key region to understanding the Paleozoic evolution of the southern part of the Palo-Asian Ocean. Here we present an integrated study of zircon U Pb ages, whole-rock major and trace elements and Sr Nd isotopes on Silurian and Late Carboniferous intermediate-felsic intrusions exposed in the Oxidaban area located in the South Tianshan region in Xinjiang, NW China....
1 CitationsSource
12345678910