Zobrazeno 1 - 10
of 35
pro vyhledávání: '"Fa-Bin Pan"'
Publikováno v:
Earth and Space Science, Vol 8, Iss 11, Pp n/a-n/a (2021)
Abstract Cenozoic volcanic rocks in the East Asian continental margin usually form because of asthenosphere upwelling and resultant decompression melting, and their origins are important in deciphering mantle geodynamics attributed to intraplate volc
Externí odkaz:
https://doaj.org/article/fa246919c3b547409ec9f5b65116dc52
Publikováno v:
Earth and Planetary Physics, Vol 3, Iss 1, Pp 62-68 (2019)
The Tibetan Plateau, known as “the roof of the world” and “the third pole of the earth”, is a product of the collision between India and Asia during the last ~50 Ma. The regional tectonics–in particular, growth and expansion of the plateau
Externí odkaz:
https://doaj.org/article/cd618a18fe1c4061a8c3e5d3c22171ed
Publikováno v:
Earth and Space Science, Vol 8, Iss 11, Pp n/a-n/a (2021)
Cenozoic volcanic rocks in the East Asian continental margin usually form because of asthenosphere upwelling and resultant decompression melting, and their origins are important in deciphering mantle geodynamics attributed to intraplate volcanism. In
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::906cbbbc6a65ba77879bb3ce3c4086c8
https://doi.org/10.1029/2020ea001324
https://doi.org/10.1029/2020ea001324
Publikováno v:
GSA Bulletin. 132:1514-1536
Two Cretaceous granitoid belts (i.e., the northwest and southeast belts) have been identified in Zhejiang, northeast South China Block. In this study, seven granitoid plutons from both the two belts were collected for zircon U-Pb dating, whole-rock g
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4a014d32ed2829efaf56c3901fc7aa77
https://doi.org/10.1130/b35426.1
https://doi.org/10.1130/b35426.1
Autor:
Lu Tao, Liqi Zhang, Liang Guo, He Yang, Hong-Fei Zhang, Chris J. Hawkesworth, Zhong Gao, Wang-Chun Xu, Biji Luo, Fa-Bin Pan
Publikováno v:
Gondwana Research. 69:177-192
High Ba-Sr granitoids occur in a number of tectonic settings, and variable petrogenetic models have been proposed. Those from post-collisional settings are rarely studied and are the focus of this study. Zircon U-Pb geochronology and whole-rock eleme
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e368a24ec9d9cb76187c744891f8e0ea
https://doi.org/10.1016/j.gr.2018.12.010
https://doi.org/10.1016/j.gr.2018.12.010
Publikováno v:
Geological Journal. 55:1064-1084
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::521c72db90858bf50f3ae29b93ba868c
https://doi.org/10.1002/gj.3444
https://doi.org/10.1002/gj.3444
Publikováno v:
Earth and Planetary Physics. 3:62-68
The Tibetan Plateau, known as " the roof of the world” and " the third pole of the earth”, is a product of the collision between India and Asia during the last ~50 Ma. The regional tectonics–in particular, growth and expansion of the plateau–
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::def065d48c3558a99d1fda06fee9dcfe
https://doi.org/10.26464/epp2019007
https://doi.org/10.26464/epp2019007
Publikováno v:
Lithos. 322:166-178
As an indicator of extensional tectonic events, MORB-like magmas could provide great insights into tectonic evolution of subduction zones. In this study, we carry out an integrated study of geochronology, geochemistry and Sr Nd isotopic compositions
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8e85ca9e27daaee39dea69e674ed7a83
https://doi.org/10.1016/j.lithos.2018.10.015
https://doi.org/10.1016/j.lithos.2018.10.015
Publikováno v:
Contributions to Mineralogy and Petrology. 176
The petrogenesis of the Eocene (43–42 Ma) Nb-rich granitoid dykes from the Kohistan–Ladakh island arc provides insights into melting of the down-going Indian continental crust during the Indian-Eurasian continental collision. These Nb-rich granit
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::11771fef8b79754acaaf17e1861c0ae9
https://doi.org/10.1007/s00410-021-01779-4
https://doi.org/10.1007/s00410-021-01779-4
Porphyries, closely associated with the copper ore deposits in orogenic belts, are usually considered to have high oxygen fugacity and display high Sr/Y ratios. However, it is still ambiguous whether the high oxygen fugacity and the enrichment of cop
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52dff877b5270ff3c37ea3e51830b1b0
https://doi.org/10.5194/egusphere-egu2020-20630
https://doi.org/10.5194/egusphere-egu2020-20630
