Zobrazeno 1 - 10
of 408
pro vyhledávání: '"Fu-Yuan Wu"'
Publikováno v:
Nature Communications, Vol 15, Iss 1, Pp 1-11 (2024)
Abstract The redox state of arc mantle has been considered to be more oxidized and diverse than that of the mid-ocean ridge, but the cause of the variation is debated. We examine the redox state of the Cenozoic global arc mantle by compiling measured
Externí odkaz:
https://doaj.org/article/38bb15166e6943ada3c7d7560fa65ac2
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 25, Iss 2, Pp n/a-n/a (2024)
Abstract Subduction initiation in oceans is key to understanding regional and global plate tectonics and ocean basin dynamics; however, its genetic mechanism is still enigmatic. The most famous model that predicts intraoceanic subduction initiation a
Externí odkaz:
https://doaj.org/article/4a8883ea2fc141a19b837ccbab5a8d17
Autor:
Bin Su, Yi Chen, Zongyu Yue, Lin Chen, Ross N. Mitchell, Ming Tang, Wei Yang, Guangyu Huang, Jinghui Guo, Xian-Hua Li, Fu-Yuan Wu
Publikováno v:
Communications Earth & Environment, Vol 4, Iss 1, Pp 1-9 (2023)
Abstract Orbital observations of non-mare, highly silicic volcanic constructs on the Moon challenge the conventional view of the formation of silicic crusts in the presence of water and plate tectonics—the former the Moon has in very short supply a
Externí odkaz:
https://doaj.org/article/d28455669fa2498395b320af2bdf554a
Autor:
Chuan-Zhou Liu, Fu-Yuan Wu, Tong Liu, Chang Zhang, Wei-Qi Zhang, Zhen-Yu Zhang, Zhen Zhang, Wu Wei, Yin-Zheng Lin
Publikováno v:
Fundamental Research, Vol 2, Iss 1, Pp 74-83 (2022)
As relics of ancient ocean lithosphere, ophiolites are the most important petrological evidence for marking the sutures and also play a key role in reconstructing plate configuration. They also provide valuable windows for studying crustal accretion
Externí odkaz:
https://doaj.org/article/ad4ef337d7af479ebc8309a070e219ac
Publikováno v:
Frontiers in Earth Science, Vol 10 (2022)
Radiogenic isotopes of granitoids are widely applied to fingerprint the source of granitoids and study the magma mingling and assimilation processes, aiming to decipher the planetary differentiation. This weapon is based on the assumption that crusta
Externí odkaz:
https://doaj.org/article/26f692d313eb4bd8a02d9962b70abd3c
Autor:
Tong Liu, Henry J. B. Dick, Chuan‐Zhou Liu, Fu‐Yuan Wu, Wen‐Bin Ji, Chang Zhang, Wei‐Qi Zhang, Zhen‐Yu Zhang, Yin‐Zheng Lin, Zhen Zhang
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 3, Pp n/a-n/a (2021)
Abstract The internal structure of oceanic crusts is not well understood due to the limitation of deep drilling. However, that of ophiolites, i.e., on‐land ancient analogs of oceanic lithosphere, could be precisely mapped and measured. The Xigaze o
Externí odkaz:
https://doaj.org/article/8d78aa6a38234e86b53b7c20aac3c4aa
Autor:
Han Zhao, Xin-Miao Zhao, P. J. Le Roux, Wen Zhang, Hao Wang, Lie-Wen Xie, Chao Huang, Shi-Tou Wu, Jin-Hui Yang, Fu-Yuan Wu, Yue-Heng Yang
Publikováno v:
Frontiers in Chemistry, Vol 8 (2020)
Clinopyroxene is a major host mineral for lithophile elements in the mantle lithosphere, and therefore, its origin is vital for constraints on mantle evolution and melt generation. In situ Sr isotopic measurement of clinopyroxene has been available s
Externí odkaz:
https://doaj.org/article/c6a8bdaa66be44339ac86a1d90fec04b
Autor:
Wei-Qiang Ji, Fu-Yuan Wu, Jia-Min Wang, Xiao-Chi Liu, Zhi-Chao Liu, Zhiyong Zhang, Wenrong Cao, Jian-Gang Wang, Chang Zhang
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
Although the Himalayan orogenic belt is dominant by Oligocene to Miocene leucogranites, it initiated magmatic activity from middle Eocene. However, the exact distribution and genesis of early magmatism are yet to be resolved. This study identified ne
Externí odkaz:
https://doaj.org/article/5e57a09216524fd59c4dc9817919e1e3
Publikováno v:
Journal of Asian Earth Sciences: X, Vol 3, Iss , Pp 100025- (2020)
Externí odkaz:
https://doaj.org/article/7898f2adf33742e58ce7cfebb7a51543
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