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Yuwang Wang
Chinese Academy of Sciences
35Publications
8H-index
237Citations
Publications 36
Newest
#1Hongjing XieH-Index: 2
#2Yuwang WangH-Index: 8
Last.Guo-Chao Zhou (China University of Geosciences)
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Abstract Massive “Pale Microgranular Masses” (PMMs) with mafic to ultramafic compositions have been discovered in representative chromite deposits (i.e., the Sartohay, Jingyu, Tangbale, Saleinuohai, Hongguleleng and Qingshui deposits) and related ophiolite belts. Based on a detailed study of the occurrence, petrology (alteration minerals) and whole-rock geochemistry, these PMMs can be subdivided into six categories: (olivine-rich) vitrobasaltic rocks, gabbro-diabasic rocks, ultramafic rocks, tuf...
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#1Yuwang WangH-Index: 8
#2Hongjing XieH-Index: 2
Last.Guo-Chao Zhou (China University of Geosciences)
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#1Lutong Zhao (Kunming University of Science and Technology)H-Index: 1
#2Jingbin WangH-Index: 2
Last.Zhi-Yuan Sun (China University of Geosciences)H-Index: 1
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Abstract The Suoerkuduke Cu−Mo skarn deposit is located in Fuyun County, Xinjiang Uygur Autonomous Region in NW China, within the northern margin of the East Junggar block. Comprehensive studies of ore deposits demonstrate that the deposit features two episodes of skarn mineralization: the first (Episode A) skarn is stratiform or lenticular and is characterized by predominantly disseminated Fe–Cu–Mo ores, whereas the second (Episode B) skarn occurs as veins or stockworks and contains predominant...
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#1Yu Shi (CUTe: China University of Technology)
#2Yuwang WangH-Index: 8
Last.Hongjing XieH-Index: 2
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Abstract An Fe-Ti-V-P ore deposit hosted by the Yaxi layered gabbroic intrusion was recently discovered in eastern Tianshan of the Central Asian Orogenic Belt (CAOB). The Yaxi intrusion is composed of interlayered leucogabbro and melagabbro, and the Fe-Ti-V-P ore layers are mainly hosted at the bottom of the melagabbro layers. We have studied the geology, petrology, mineralogy and geochemistry of the Yaxi gabbroic rocks and associated ore. Igneous zircons separated from a gabbro sample yield a S...
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#1Zhi-Yuan SunH-Index: 1
#2Jingbin WangH-Index: 4
Last.Meng-Long WangH-Index: 1
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Abstract The volcanic rocks hosting the iron deposits in the Aqishan–Yamansu metallogenic belt are sodium-rich. The geochronology, petrography, and geochemistry of minerals and sodium-rich rocks as well as the relationship between these rocks and the iron deposits are studied. Geochemically, the ore-hosting volcanic rocks are sodium-rich (the averages of Na2O and Na2O/K2O are 4.31 ​wt.% and 8.56, respectively) and belong to the calc-alkaline series. They are enriched in LREEs and LILEs (Ba, U, K...
1 CitationsSource
#1Yan SunH-Index: 7
#2Jingbin WangH-Index: 4
Last.Lingli LongH-Index: 4
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Abstract The early Permian Cu–Ni sulfide-bearing mafic-ultramafic intrusions from North Xinjiang in NW China help to provide constraints on the late Paleozoic crustal growth in the Central Asian Orogenic Belt (CAOB) and improve the understanding of the genesis of magmatic sulfide mineralization in orogenic settings and the identification of future prospecting targets. The Cu–Ni sulfide-mineralized Yueyawan gabbroic complex in Kalatag represents a new breakthrough for Cu–Ni prospecting in covered...
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#1Mingjie Yu (SCNU: South China Normal University)H-Index: 2
#2Yuwang WangH-Index: 8
Last.Rui Zhang (China University of Geosciences)H-Index: 2
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Abstract The Kalatage area, located in the middle of the Dananhu arc in the Eastern Tianshan, NW China, contains abundant and different types of mineralization, e.g. volcanogenic massive sulfide (VMS) Cu-Zn deposits, porphyry Cu (-Au) deposits and volcanic hydrothermal vein Cu (-Au) deposits, represents an integral component of the Central Asian Orogenic Belt (CAOB). The Meiling hydrothermal Cu-Zn (-Au) deposit is located in the core of the Kalatage area and can be studied to better understand t...
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#1Yan SunH-Index: 7
#2Jingbin WangH-Index: 4
Last.Mingjie YuH-Index: 2
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Abstract The pre-Carboniferous evolution of the Eastern Tianshan orogen, Xinjiang, NW China, an important Paleozoic tectonic component and Cu metallogenic belt in the southern Central Asian Orogenic Belt (CAOB), is controversial. New zircon U Pb ages, whole-rock geochemistry, and zircon Lu Hf isotope data for three major granitic complexes (i.e., Kalatag, Dongerqu, Xierqu) from the Kalatag Cu cluster of Eastern Tianshan were combined with previous data to evaluate Ordovician–Devonian arc evoluti...
2 CitationsSource
#1Zhi-Yuan Sun (China University of Geosciences)H-Index: 1
#2Lingli LongH-Index: 4
Last.Meng-Long WangH-Index: 1
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Abstract The Hongyuntan magnetite deposit, which is located in the Aqishan–Yamansu belt of Eastern Tianshan, Xinjiang, is hosted within Carboniferous submarine volcanic-sedimentary sequences. The deposit is characterized by five metallogenic stages: Stage I (garnet–diopside), Stage II (magnetite–tremolite–chlorite–pyrite), Stage III (magnetite–quartz–albite–actinolite), Stage IV (pyrite–quartz–epidote) and Stage V (hematite–limonite). Pyrite associated with magnetite formed during the Stage II h...
1 CitationsSource
#1Lutong ZhaoH-Index: 1
#2Jingbin WangH-Index: 4
Last.Chao LiH-Index: 2
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Abstract The Sareke Cu deposit in the western Tarim region (Xinjiang, NW China) is hosted in continental sedimentary rocks of the Upper Jurassic Kuzigongsu Formation and Lower Cretaceous Kezilesu Group. Stratabound orebodies occur mainly in conglomerate and minor in siltstone. Both stratabound (major) and vein type (minor) ores are composed of chalcocite, chalcopyrite, bornite and pyrite with minor sphalerite and galena, which show a zonation pattern of chalcocite → chalcopyrite → sphalerite + g...
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