Zobrazeno 1 - 10
of 50
pro vyhledávání: '"Xiu-Zheng Zhang"'
Autor:
Jing‐Jing Fan, Qiang Wang, Gang‐Jian Wei, Jie Li, Lin Ma, Xiu‐Zheng Zhang, Zi‐Qi Jiang, Jin‐Long Ma, Jin‐Sheng Zhou, Qi‐Wei Li, Zi‐Long Wang, Xiao Liu, Tong‐Yu Huang, Miao‐Yan Zhang
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 24, Iss 6, Pp n/a-n/a (2023)
Abstract The origins of Cenozoic granites in the Himalaya are key to understanding the evolution of the Himalayan orogen. However, it is unclear whether these granites represent primary melts, and the nature of their magma source is controversial. He
Externí odkaz:
https://doaj.org/article/41f2d24e24a142109fddf6bcb21ed1b8
Autor:
Chuan-Bing Xu, Ji-Peng Zeng, Qiang Wang, Xiu-Zheng Zhang, Quan Ou, Jun Wang, Lu-Lu Hao, Yiwei Chen
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
The timing and mechanism of crustal thickening and initial surface uplift of the Tibetan Plateau remain disputed. Here, we report zircon U–Pb geochronological and O isotopic and whole-rock geochemical and Sr–Nd isotopic data for Eocene (41–37 M
Externí odkaz:
https://doaj.org/article/601cbe139d0149ee8ea7b86b62353500
Autor:
Qiang Wang, Chris J. Hawkesworth, Derek Wyman, Sun-Lin Chung, Fu-Yuan Wu, Xian-Hua Li, Zheng-Xiang Li, Guo-Ning Gou, Xiu-Zheng Zhang, Gong-Jian Tang, Wei Dan, Lin Ma, Yan-Hui Dong
Publikováno v:
Nature Communications, Vol 7, Iss 1, Pp 1-11 (2016)
The role of the low velocity-high conductivity zones (LV–HCZs) in developing the Tibetan Plateau has remained controversial. Here, Wang et al.present new geochemical and petrological data that show the LV–HCZs are sources of partial melt thus giv
Externí odkaz:
https://doaj.org/article/73d278f1984c4e5f9987bfcdfc237105
Publikováno v:
Geology. 50:1432-1437
Partial melting during high-temperature to ultrahigh-temperature (UHT) metamorphism facilitates crustal differentiation, element transfer, and the evolution of topography in orogens, however the mechanisms that drive heating of Earth’s crust remain
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::736dd5d03a26bb281e943dbf7ef99bae
https://doi.org/10.1130/g50387.1
https://doi.org/10.1130/g50387.1
Publikováno v:
Geochimica et Cosmochimica Acta. 334:241-258
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::12d2d0aeb0f7d58b57c3d3ea093e3236
https://doi.org/10.1016/j.gca.2022.08.009
https://doi.org/10.1016/j.gca.2022.08.009
Autor:
Jing-Jing Fan1,2, Xiu-Zheng Zhang1,3 zhangxz@gig.ac.cn, Lin Ma1,3, Qiang Wang1,2,3, Zi-Qi Jiang4, Xiao-Ping Xia1,3, Gang-Jian Wei1,3, Zi-Long Wang1,2, Jin-Sheng Zhou1,3, Qi-Wei Li5, Xiao Liu4, Tong-Yu Huang1,2, Miao-Yan Zhang1,2, Jin-Heng Liu1,2
Publikováno v:
Geological Society of America Bulletin. Jan/Feb2024, Vol. 136 Issue 1/2, p433-446. 14p.
Autor:
Jing-Jing Fan, Xiu-Zheng Zhang, Lin Ma, Qiang Wang, Zi-Qi Jiang, Xiao-Ping Xia, Gang-Jian Wei, Zi-Long Wang, Jin-Sheng Zhou, Qi-Wei Li, Xiao Liu, Tong-Yu Huang, Miao-Yan Zhang, Jin-Heng Liu
Publikováno v:
GSA Bulletin.
Large-scale N-S shortening induced by India-Asia convergence caused the formation of numerous E-W−trending mountain ranges in Tibet. However, the mechanism(s) of formation of N-S−trending mountain ranges remains elusive. We report on a felsic mag
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9cbd2a120ee2ad9c8e30a8b83b6b08d0
https://doi.org/10.1130/b36617.1
https://doi.org/10.1130/b36617.1
Publikováno v:
GSA Bulletin. 135:67-80
The debate over global continental reorganization from Rodinia to Gondwana likely stems from some key Neoproterozoic units being overlooked in previous reconstructions. Here we provide a self-consistent set of evidence, based on magmatism and metamor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::03c1f74b77ddd92bb9562d50808228c4
https://doi.org/10.1130/b36152.1
https://doi.org/10.1130/b36152.1
Autor:
Xiu-Zheng Zhang, Qiang Wang, Derek Wyman, Quan Ou, Yue Qi, Guo-Ning Gou, Wei Dan, Ya-Nan Yang
Publikováno v:
Geology. 50:610-614
The topographic transition of central–northern Tibet since the early Miocene has created a consistently high and flat plateau similar to that of today. However, to date, the associated deep crust and/or /mantle events are poorly understood, mainly
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f0ed0cc9d84f42b9e587a0fc4d02edcd
https://doi.org/10.1130/g49534.1
https://doi.org/10.1130/g49534.1
Publikováno v:
Geological Society, London, Special Publications. 531
An evaluation of the potential geodynamic connections between the evolution of Paleozoic oceans in NW Gondwana and NE Gondwana is challenging. Until recently, most syntheses emphasized only two Paleozoic oceans (the Proto-Tethys and the Palaeo-Tethys
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8699ac2b45b57a41c12d088331f1a493
https://doi.org/10.1144/sp531-2022-146
https://doi.org/10.1144/sp531-2022-146