Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Jintuan Wang"'
Publikováno v:
Solid Earth Sciences, Vol 8, Iss 4, Pp 283-294 (2023)
Metasomatic zircons in ultramafic rocks are crucial in tracking orogenic processes. Metasomatic zircons are conceived to form by local zircon saturation resulting from effective Zr transport during metamorphic events and incomplete Zr accommodation i
Externí odkaz:
https://doaj.org/article/84229d0698a4472ea21848bfc3559204
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-7 (2022)
The basalt V-Ti redox proxy indicates that both of the Archean ambient and modified mantle exhibit a ~1.0 log unit increase in their evolution for most cratons, possibly derived by widespread crustal recycling.
Externí odkaz:
https://doaj.org/article/3452cfc12b9c4a429c478a145cdef155
Publikováno v:
Geochimica et Cosmochimica Acta. 333:107-123
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7a7555c530cc5a97376cb371ed626909
https://doi.org/10.1016/j.gca.2022.07.004
https://doi.org/10.1016/j.gca.2022.07.004
Redox evolution during arc magma differentiation revealed by mineral/melt Fe3+ and Fe2+ partitioning
The oxidizing capacity of volcanic gases relies on both the redox state of the mantle and the redox evolution of mantle-derived magmas. Arc magmas transfer abundant volatiles from the mantle and undergo extensive differentiation before degassing. But
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3b264734361e2c24379ea7127d423316
https://doi.org/10.21203/rs.3.rs-1540804/v1
https://doi.org/10.21203/rs.3.rs-1540804/v1
Publikováno v:
Science China Earth Sciences. 63:1952-1968
Oxygen fugacity (fO2) is an intensive variable that describes the redox state of a system. By controlling the valence state of multivalent elements, fO2 affects the stability of iron-bearing minerals, dominants the species of volatile elements (e.g.,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a7f7c390d71b47cdb947d8c05f613b8c
https://doi.org/10.1007/s11430-019-9662-2
https://doi.org/10.1007/s11430-019-9662-2
Autor:
Li Li, Lei Zhang, Jianping Li, Ting Xu, Xingcheng Liu, Xiaolin Xiong, Zhongxing Sun, Jintuan Wang, Fangfang Huang, Mengfei Ruan, Wei Chen
Publikováno v:
Science China Earth Sciences. 63:1938-1951
The partitioning behavior of trace elements is of key importance for understanding the geochemical process and material cycle mechanism in subduction zones. This paper focuses on the advances and prospects on the studies of trace element partitioning
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4926e8cbf658d1e98832e7fdba7ab262
https://doi.org/10.1007/s11430-019-9631-6
https://doi.org/10.1007/s11430-019-9631-6
The redox evolution of Archean mantle impacted Earth differentiation, mantle melting and the nature of chemical equilibrium between mantle, ocean and atmosphere of the early Earth. However, how and why it varies with time remain controversial. Archea
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::11fb6410d34f65a25964223b2705254f
https://doi.org/10.21203/rs.3.rs-948127/v1
https://doi.org/10.21203/rs.3.rs-948127/v1
Publikováno v:
Journal of Geophysical Research: Solid Earth. 124:4617-4638
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::21d1baf0385863dee904f02569a34105
https://doi.org/10.1029/2018jb016731
https://doi.org/10.1029/2018jb016731
Publikováno v:
Journal of Geophysical Research: Biogeosciences. 125
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::301c8ae05182e1c44694204014c33d58
https://doi.org/10.1029/2020jg005735
https://doi.org/10.1029/2020jg005735
Autor:
Xiaolin Xiong, Linli Chen, Jintuan Wang, Michael J. Walter, Eiichi Takahashi, Li Li, Toshihiro Suzuki
Publikováno v:
Journal of Geophysical Research: Solid Earth. 125
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b9f99b2185e8ff58f1324979253f8728
https://doi.org/10.1029/2020jb019452
https://doi.org/10.1029/2020jb019452