Zobrazeno 1 - 10
of 21
pro vyhledávání: '"Si‐Fang Huang"'
Publikováno v:
China Geology, Vol 4, Iss 2, Pp 367-370 (2021)
Externí odkaz:
https://doaj.org/article/bd1146b6dd30431bb04dce58012ce3ff
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 22, Iss 11, Pp n/a-n/a (2021)
Abstract Subduction initiation processes, such as those evidenced in the Izu‐Bonin‐Mariana (IBM) forearc crust are a key feature of modern‐style plate tectonics. However, the evidence for this process in the Precambrian is limited, due to the s
Externí odkaz:
https://doaj.org/article/330ea19a522448a385cd8ee72640cdf9
Autor:
Bin Huang, Wei Wang, Jun-Hong Zhao, Nimat Ullah Khattak, Si-Fang Huang, Gui-Mei Lu, Er-Kun Xue, Li Sun
Publikováno v:
Geological Society of America Bulletin.
The newly identified Neoproterozoic Yuanmou high-Nb mafic and adakitic rocks at the western margin of the Yangtze Block in South China are investigated for petrogenesis and geodynamic implications. Zircon U-Pb ages show the adakitic granodiorite host
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b999fa336cda9f9ce95746e6191c8b44
https://doi.org/10.1130/b36618.1
https://doi.org/10.1130/b36618.1
Publikováno v:
China Geology. 4:1-4
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f7c613d0b44a53a672493fbeeb25d495
https://doi.org/10.31035/cg2021007
https://doi.org/10.31035/cg2021007
Publikováno v:
GSA Bulletin. 133:717-739
The role of the Cathaysia Block, South China, and its linkage with orogenesis in the Rodinia and Gondwana supercontinents remain unresolved because of uncertainties in its paleoposition in supercontinental reconstructions. The lithostratigraphic, geo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1f16a20f56941e871646d9e65da35b06
https://doi.org/10.1130/b35588.1
https://doi.org/10.1130/b35588.1
Publikováno v:
Geochemistry, Geophysics, Geosystems. 22
Subduction initiation processes, such as those evidenced in the Izu-Bonin-Mariana (IBM) forearc crust are a key feature of modern-style plate tectonics. However, the evidence for this process in the Precambrian is limited, due to the scarcity of ophi
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b6c99830348af875e7ab031acbfef135
https://doi.org/10.1029/2021gc010137
https://doi.org/10.1029/2021gc010137
Publikováno v:
Lithos. :45-58
The Neoproterozoic Jiangnan Orogenic Belt in south China was formed by the amalgamation of the Yangtze and Cathaysia blocks, however, the timing of its formation is still debated. In this study, we present whole rock geochemistry, U-Pb zircon ages, L
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::234cd29607896e52f30c51a48e22423b
https://doi.org/10.1016/j.lithos.2019.05.016
https://doi.org/10.1016/j.lithos.2019.05.016
Publikováno v:
Lithos. :23-38
The fragmentation of the Columbia supercontinent is thought to have begun as early as ~1.7 Ga; however, the breakup of its core domain occurred only at ~1.5–1.25 Ga. This study presents the integrated petrological and chemical characteristics of ga
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::37e729cbb05fcb3f9e83cbd2bfa514fb
https://doi.org/10.1016/j.lithos.2019.02.021
https://doi.org/10.1016/j.lithos.2019.02.021
Publikováno v:
Precambrian research. 2019. Vol. 322. P. 66-84
Three episodes of mafic magmatism are identified by zircon and baddeleyite U-Pb dating at 2299 ± 17 Ma, 1703 ± 8 Ma and 1511 ± 14 Ma in the southwestern Yangtze Block. These mafic rocks have tholeiitic compositions with enrichment of LILE but an a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b0cc8e37974f6b1f0aa8b667438f9312
https://doi.org/10.1016/j.precamres.2018.12.019
https://doi.org/10.1016/j.precamres.2018.12.019
Autor:
Bovari Syprien Yomeun, Wei Wang, Jean Pierre Tchouankoue, Michele Sandra Kamguia Kamani, Kevin Igor Azeuda Ndonfack, Si-Fang Huang, Emmanuel Archelaus Afanga Basua, Gui-Mei Lu, Er-Kun Xue
Publikováno v:
Lithos. :106700
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::27bada9850eff2f5d7f27e121de56e33
https://doi.org/10.1016/j.lithos.2022.106700
https://doi.org/10.1016/j.lithos.2022.106700