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Jiang-Bo Wang
Northwest University (United States)
5Publications
2H-index
16Citations
Publications 5
Newest
#1Zezhong Zhang (Northwest University (United States))H-Index: 1
#2Jiang-Feng Qin (Northwest University (United States))H-Index: 12
Last.Jiang-Bo Wang (Northwest University (United States))H-Index: 2
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#1Jiang-Feng Qin (Northwest University (United States))H-Index: 12
#2Shaocong Lai (Northwest University (United States))H-Index: 19
Last.Zezhong Zhang (Northwest University (United States))H-Index: 1
view all 9 authors...
#1Shaocong Lai (Northwest University (United States))H-Index: 19
#2Jiang-Feng Qin (Northwest University (United States))H-Index: 12
Last.Jiang-Bo Wang (Northwest University (United States))H-Index: 2
view all 10 authors...
#1Ren-Zhi Zhu (Northwest University (United States))H-Index: 8
#2Shaocong Lai (Northwest University (United States))H-Index: 19
Last.Jiang-Bo Wang (Northwest University (United States))H-Index: 2
view all 5 authors...
Abstract Geochemical variations in granitic rocks may be controlled by their source rocks, melting reactions and subsequent magmatic processes, which resulted from various geodynamic processes related to subduction, collision, or slab break-off. Here we report new LA–ICP-MS zircon U–Pb ages and Hf isotopes, whole-rock chemistry and Sr–Nd isotopes for the late Early Cretaceous quartz diorite, granodiorite and monzogranite in the Gaoligong belt, southeastern Tibet Plateau. The zircon U–Pb dating y...
#1Shao-Wei Zhao (Northwest University (United States))H-Index: 8
#2Shaocong Lai (Northwest University (United States))H-Index: 19
Last.Jiang-Bo Wang (Northwest University (United States))H-Index: 2
view all 5 authors...
Abstract The Tengchong Block of Southwestern China is key to tracing the eastward subduction of Neo-Tethys and collision between Indian and Asian continents. The block contains a magmatic belt that represents the southeastward continuation of the Gangdese belt, produced by the eastward subduction of eastern Neo-Tethyan oceanic lithosphere. In this paper we present geochemical and geochronological data of Late Cretaceous to Early Paleocene (~ 64 Ma) granitic rocks of the Guyong and Husa batholith...
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