Genesis of the Xianghualing Sn–Pb–Zn deposit, South China: a multi-method zircon study
Abstract The Xianghualing Sn–Pb–Zn deposit is situated near the center of the world-class
Nanling W–Sn ore belt, associated with the highly evolved Laiziling granite of Jurassic age …
Nanling W–Sn ore belt, associated with the highly evolved Laiziling granite of Jurassic age …
[HTML][HTML] Contrasting Nb-Ta mineralization between the Mufushan and Lianyunshan granites, South China: Evidence from whole-rock and zircon geochemistry and …
Abstract The Mufushan (MFS) and Lianyunshan (LYS) granitic complexes are located in
northeastern Hunan (South China) and host important Nb-Ta mineralization. Fine-grained …
northeastern Hunan (South China) and host important Nb-Ta mineralization. Fine-grained …
The timing of collision between Asia and the West Burma Terrane, and the development of the Indo‐Burman Ranges
Abstract The West Burma Terrane (WBT) is a small terrane bounded to the east by the Asian
Sibumasu Block and to the west by the Indo‐Burman Ranges (IBR), the latter being an …
Sibumasu Block and to the west by the Indo‐Burman Ranges (IBR), the latter being an …
[HTML][HTML] Long-lived Nb-Ta mineralization in Mufushan, NE Hunan, South China: geological, geochemical, and geochronological constraints
Abstract The Mufushan Complex (MFSC), located in northeastern Hunan, is a significant
producer of Nb-Ta-Li-Be rare metals in South China. The present study examines the …
producer of Nb-Ta-Li-Be rare metals in South China. The present study examines the …
Timing and origin of multi-stage magmatism and related W–Mo–Pb–Zn–Fe–Cu mineralization in the Huangshaping deposit, South China: an integrated zircon study
Abstract The Huangshaping deposit (South China) is closely related to hypabyssal granites
(eg, quartz porphyry, granophyre, and granite porphyry), developing massive skarn-type W …
(eg, quartz porphyry, granophyre, and granite porphyry), developing massive skarn-type W …
Two-stage CuPbZn mineralization of the Baoshan deposit in southern Hunan, South China: Constraints from zircon and pyrite geochronology and geochemistry
Abstract The Baoshan Cusingle bondPbsingle bondZn deposit is one of the representative
polymetallic deposits in the middle of the Nanling Range, the western part of the Qin–Hang …
polymetallic deposits in the middle of the Nanling Range, the western part of the Qin–Hang …
Zircon indicators of fluid sources and ore genesis in a multi-stage hydrothermal system: The Dongping Au deposit in North China
The syenite-hosted Dongping gold deposit represents the largest gold deposit on the
northern margin of the North China Craton. Here, we present new U single bond Pb age …
northern margin of the North China Craton. Here, we present new U single bond Pb age …
Co-development of Jurassic I-type and A-type granites in southern Hunan, South China: Dual control by plate subduction and intraplate mantle upwelling
Two types of spatially and temporally associated Jurassic granitic rocks, I-type and A-type,
occur as pluton pairs in several locations in southern Hunan Province, South China. This …
occur as pluton pairs in several locations in southern Hunan Province, South China. This …
Combined zircon, molybdenite, and cassiterite geochronology and cassiterite geochemistry of the Kuntabin tin-tungsten deposit in Myanmar
W Mao, H Zhong, J Yang, Y Tang, L Liu… - Economic …, 2020 - pubs.geoscienceworld.org
Abstract The Kuntabin Sn-W deposit, located in southern Myanmar, is characterized by
abundant greisen-type and quartz vein-type cassiterite and wolframite mineralization. We …
abundant greisen-type and quartz vein-type cassiterite and wolframite mineralization. We …
Rare earth element enrichment in the ion-adsorption deposits associated granites at Mesozoic extensional tectonic setting in South China
Ion-adsorption type rare earth element mineralization occurs in weathered profile of three
Mesozoic granites in the Bachi area, Guangdong Province, South China. In this study, we …
Mesozoic granites in the Bachi area, Guangdong Province, South China. In this study, we …