Branding/Logomark minus arrow-point-to-down Citation Combined Shape Icon/Bookmark-empty Icon/Copy Icon/Collection Icon/Close Copy 7 Icon/List no author result Created with Sketch.
Loading Scinapse...
Qingfei Wang
China University of Geosciences
86Publications
23H-index
1,532Citations
Publications 86
Newest
Xuefei Liu11
Estimated H-index: 11
(China University of Geosciences),
Pengfei Zuo + 3 AuthorsDeshun Zheng
ABSTRACT Whether the North Qinling Terrane (NQT) was accreted to the North China Craton (NCC) in the Proterozoic is still a matter of debate. We report the first detrital zircon study from the Baishugou Formation, which forms the uppermost part of the Mesoproterozoic Guandaokou Group, at the southernmost NCC margin. Detrital zircons from carbonaceous silty phyllite in the lower part of the Baishugou Formation yield U–Pb ages peaking at ca. 2500 Ma, with minor peaks at ca. 2300–2000, 1800, and 16...
Source Cite
Fangge Chen1
Estimated H-index: 1
(China University of Geosciences),
Qingfei Wang23
Estimated H-index: 23
(China University of Geosciences)
+ 4 AuthorsEmmanuel John M. Carranza44
Estimated H-index: 44
(James Cook University)
ABSTRACTThe evolution of the Palaeo-Tethys Ocean played an important role in the Palaeozoic tectono-metallogenesis in Southeast Asia, in which diverse blocks amalgamated due to its closure. Previous researches focused mostly on endogenic metallogenesis related to the evolution of the Palaeo-Tethys Ocean. However, the tectonic control on the numerous Mn ore deposits in the southwestern South China Block (SCB) developed during Palaeo-Tethys evolution is largely unknown. In this article, we review ...
1 Citations Source Cite
2018 in LithosIF: 3.86
Zhen Zheng4
Estimated H-index: 4
(Peking University),
Yan-Jing Chen36
Estimated H-index: 36
(Peking University)
+ 3 AuthorsQingfei Wang23
Estimated H-index: 23
(China University of Geosciences)
Abstract The Qiman Tagh of the East Kunlun Orogen, NW China, lies within the Tethysides and hosts a large W–Sn belt associated with the Bashierxi monzogranite. To constrain the origin of the granitic magmatism and its relationship with W–Sn mineralization and the tectonic evolution of the East Kunlun Orogen and the Tethys, we present zircon U–Pb ages and Hf isotopic data, and whole-rock compositional and Sr–Nd–Pb isotopic data of the Bashierxi monzogranite. The granite comprises quartz, K-feldsp...
4 Citations Source Cite
Lin Yang3
Estimated H-index: 3
,
Rui Zhao + 2 AuthorsEmmanuel John M. Carranza44
Estimated H-index: 44
Abstract The structures and fluid-rock reaction in the Xinli gold deposit, Jiaodong Peninsula, were investigated to further understand their combined controls on the development of permeability associated with ore-forming fluid migration. Orebodies in this deposit are hosted by the moderately SE-to S-dipping Sanshandao–Cangshang fault (SCF). Variations in both dip direction and dip angle along the SCF plane produced fault bends, which controlled the fluid accumulation and ore-shoot formation. Go...
Source Cite
2018 in LithosIF: 3.86
Yayun Liang4
Estimated H-index: 4
(China University of Geosciences),
Jun Deng29
Estimated H-index: 29
(China University of Geosciences)
+ 7 AuthorsJiang1
Estimated H-index: 1
Abstract Early Cretaceous mafic dyke swarms are widely developed on Jiaodong Peninsula in the southeastern part of the North China Craton (NCC), but their petrogenesis remains enigmatic. We have examined the in-situ major element, trace element and Sr isotope compositions of the clinopyroxene phenocrysts in these dykes in order to evaluate the extent of magma mixing and source metasomatism. Depending on the type of mineral zoning, the clinopyroxene phenocrysts in our samples can be classified in...
1 Citations Source Cite
Jiahao Chen1
Estimated H-index: 1
(China University of Geosciences),
Qingfei Wang23
Estimated H-index: 23
(China University of Geosciences)
+ 2 AuthorsJiaqi Wang1
Estimated H-index: 1
(China University of Geosciences)
Abstract Iron-rich gibbsitic bauxite, located in the Yongjiang basin, southwestern part of South China Block, characterized by nodules mixed with loose clayey soil. Bauxite ores consist of gibbsite, kaolinite, hematite and goethite and few zircon and quartz. The nodules have higher ratios of Al/Si and stronger ferrallitization compared to the enclosing soil. The nodules have a lower content of Rb and Cs that were easily depleted during the weathering process, and a higher content of Ga, Sc, V, C...
3 Citations Source Cite
2018 in Ore Geology ReviewsIF: 3.99
Zhen Zheng1
Estimated H-index: 1
(China University of Geosciences),
Yan-Jing Chen36
Estimated H-index: 36
(Peking University)
+ 3 AuthorsQingfei Wang23
Estimated H-index: 23
(China University of Geosciences)
Abstract The Qiman Tagh W-Sn ore belt is located in the westernmost sector of the East Kunlun Orogen, NW China. It has been recognized as a unique W-Sn belt that formed in the early Paleozoic and related to closure of the Proto-Tethys. To understand the evolution of ore-forming fluids and its relationship with the tectonic setting of East Kunlun Orogen, we report the results obtained from fluid inclusion and H-O isotopic studies of ores and quartz veins for the Qiman Tagh W-Sn ore belt. Minerali...
1 Citations Source Cite
2018 in Ore Geology ReviewsIF: 3.99
Fuchuan Chen2
Estimated H-index: 2
(China University of Geosciences),
Jun Deng29
Estimated H-index: 29
(China University of Geosciences)
+ 5 AuthorsRong Xu (China University of Geosciences)
Abstract The Heiniuwa gold deposit is located in the northwestern segment of the Longyang Au–Fe–Pb–Zn polymetallic ore cluster in the northern Baoshan block, Sanjiang region, SW China. This ore cluster is characterized by skarn Fe–Pb–Zn mineralization (∼120 Ma) in the central part and Au mineralization in the distal part. The genesis of the Heiniuwa deposit and its relationship with the skarn deposits remain unclear. All orebodies in Heiniuwa are hosted in the Upper Cambrian calcareous slate and...
Source Cite
2018 in Gondwana ResearchIF: 5.66
Lin Yang3
Estimated H-index: 3
(China University of Geosciences),
Qingfei Wang23
Estimated H-index: 23
(China University of Geosciences)
+ 1 AuthorsGongjian Li9
Estimated H-index: 9
(China University of Geosciences)
Abstract The Simao block, northern extension of Indochina block, was located along the Proto-Tethyan subduction zone in Early Paleozoic and subducted by the Paleo-Tethyan Ailaoshan ocean along its eastern margin in Permo-Triassic. The location of Simao block in the Proto-Tethyan paleogeography and the Permo-Triassic consumption process of the Ailaoshan ocean were unclear. Detrital zircons from Silurian to Triassic strata and the representative Xin'anzhai intrusion in the eastern margin of Simao ...
5 Citations Source Cite
123456789