Zobrazeno 1 - 10
of 43
pro vyhledávání: '"Fangyang Hu"'
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:
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
Autor:
Guozheng Sun, Shuwen Liu, Peter A. Cawood, Ming Tang, Jeroen van Hunen, Lei Gao, Yalu Hu, Fangyang Hu
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-11 (2021)
Constraining the thermal state of the lithosphere is crucial to understanding geodynamic regime in early Earth. Here the authors reconstruct ~2.9–2.5 Ga thermal structure of continental lithosphere of the North China Craton using TTG and propose a
Externí odkaz:
https://doaj.org/article/832dd3c7d0e54372be6138c6394da17b
Publikováno v:
Scientific Reports, Vol 7, Iss 1, Pp 1-10 (2017)
Abstract We present compiled geochemical data of young (mostly Pliocene-present) intermediate magmatic rocks from continental collisional belts and correlations between their whole-rock Sr/Y and La/Yb ratios and modern crustal thickness. These correl
Externí odkaz:
https://doaj.org/article/9bdf330002b14540a8e6335c924a7a86
Publikováno v:
Frontiers in Earth Science; 2024, p01-21, 21p
Autor:
Shuwen Liu, Peter Cawood, Jiachen Yao, Lei Gao, Rongrong Guo, Fangyang Hu, Denggang Lu, Xin He, Wei Wang
How Earth switched from any earlier regimes such as plume-lid tectonics to plate tectonics remains an unresolved issue in Earth sciences. We report early Neoarchean (~ 2.77–2.68 Ga) metavolcanic rocks, including older calc-alkaline basaltic-andesit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7923ffd000ba394b791c4fcc9cb368e4
https://doi.org/10.21203/rs.3.rs-2881098/v1
https://doi.org/10.21203/rs.3.rs-2881098/v1
Publikováno v:
GSA Bulletin. 134:2072-2084
Accretionary orogens function as major sites for the generation of continental crust, but the growth model of continental crust remains poorly constrained. The Central Asian Orogenic Belt, as one of the most important Phanerozoic accretionary orogens
Autor:
Jeroen van Hunen, Shuwen Liu, Peter A. Cawood, Lei Gao, Guozheng Sun, Ming Tang, Yalu Hu, Fangyang Hu
Publikováno v:
Nature Communications, Vol 12, Iss 1, Pp 1-11 (2021)
Nature Communications
Nature communications, 2021, Vol.12(1), pp.3888 [Peer Reviewed Journal]
Nature Communications
Nature communications, 2021, Vol.12(1), pp.3888 [Peer Reviewed Journal]
Constraining thickness and geothermal gradient of Archean continental crust are crucial to understanding geodynamic regimes of the early Earth. Archean crust-sourced tonalitic–trondhjemitic–granodioritic gneisses are ideal lithologies for reconst
Publikováno v:
Gondwana Research. 88:296-332
The Qinling Orogenic Belt in Central China is formed by an oblique continental collision between the North China and South China Blocks. In this review, we summarize the knowledge of the early Mesozoic magmatism, in combination with the coeval metamo
Publikováno v:
Case Studies in Thermal Engineering, Vol 60, Iss , Pp 104785- (2024)
The torque generated by high-speed airflow has a beneficial impact on a compressor disk cavity with radial inflow. The purpose of this study is to investigate the torque and energy recovery of a compressor disk cavity with tubed vortex reducer (TVR)
Externí odkaz:
https://doaj.org/article/eeaca10c805a472886e082d1dabaa50c