Výsledky vyhledávání - "Hao Y.C. Wang"

Rifting of the northern margin of the Indian craton in the Early Cretaceous: Insight from the Aulis Trachyte of the Lesser Himalaya (Nepal)

Autor: Rasoul Esmaeili, Wenjiao Xiao, Rui Li, Brian F. Windley, Hao Y.C. Wang, Rixiang Zhu, Saunak Bhandari, Songjian Ao

Publikováno v: Lithosphere. 11:643-651

To reconstruct the early tectonic history of the Himalayan orogen before final India-Asia collision, we carried out geochemical and geochronological studies on the Early Cretaceous Aulis Trachyte of the Lesser Himalaya. The trace-element geochemistry

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::2546e28f524238b76c64681a1e302986
https://doi.org/10.1130/l1058.1

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Amphibolite facies metamorphism and geochronology of the Paleoproterozoic Aketashitage Orogenic Belt, northwestern China

Autor: Chun-Ming Wu, Yichao Chen, Qian W.L. Zhang, Jia-Hui Liu, Hui C.G. Zhang, Zhen M.G. Li, Hao Y.C. Wang, Meng-Yan Shi, Van-Tho Pham

Publikováno v: Precambrian Research. 328:146-160

Garnet amphibolite and semi-pelitic gneiss preserving three stages of metamorphic mineral assemblages, i.e., the prograde metamorphic inclusion assemblage (M1) preserved in the garnet porphyroblast, metamorphic peak assemblage (M2) and retrograde sym

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::239bc5f7b6093d337458fda8b3d53fc0
https://doi.org/10.1016/j.precamres.2019.04.019

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Metamorphic evolution and SHRIMP U-Pb geochronology of mafic granulites with double symplectites in the Fuping metamorphic complex, middle Palaeoproterozoic Trans-North China Orogen

Autor: Qian W.L. Zhang, Hong-Xu Chen, Chun-Ming Wu, Hui C.G. Zhang, Jia-Hui Liu, Tao Peng, Van Tho Pham, Hao Y.C. Wang

Publikováno v: Precambrian Research. 326:142-154

Garnet-bearing mafic granulites occur as lenses within TTG gneiss or metapelite in the Fuping Complex, middle Palaeoproterozoic Trans-North China Orogen. They are composed mainly of garnet, clinopyroxene, orthopyroxene, hornblende, plagioclase, quart

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::d3bd3cd03d4c13f2418d6e9ed8d39dfc
https://doi.org/10.1016/j.precamres.2017.11.009

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Metamorphic P-T path and geochronology of garnet-bearing amphibolite of the Inyoni Shear Zone, southwestern Barberton Greenstone Belt, South Africa

Autor: Jia-Hui Liu, Hui C.G. Zhang, Hong-Xu Chen, Guo-Dong Wang, Hao Y.C. Wang, Chun-Ming Wu, Tao Peng

Publikováno v: Precambrian Research. 321:261-276

Geothermobarometry and phase equilibria modeling were conducted for garnet-bearing amphibolite of the Inyoni Shear Zone (ISZ), southwestern Barberton Greenstone Belt, South Africa. The prograde (M1), metamorphic peak (M2) and retrograde (M3) metamorp

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a29e1308ba194077c359a90b29389bc4
https://doi.org/10.1016/j.precamres.2018.12.021

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First report of ultra-high pressure metamorphism in the Paleozoic Dunhuang orogenic belt (NW China): Constrains from P-T paths of garnet clinopyroxenite and SIMS U-Pb dating of titanite

Autor: Chun-Ming Wu, Jun-Sheng Lu, Qian W.L. Zhang, Jia-Hui Liu, Meng-Yan Shi, Zhen M.G. Li, Hao Y.C. Wang

Ultra-high pressure (UHP) metamorphism is recorded by garnet clinopyroxenite enclaves enclosed in an undeformed, unmetamorphosed granitic pluton, northeastern Paleozoic Dunhuang orogenic belt, northwest China. Three to four stages of metamorphic mine

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::932935665a05c01d9a2a11b2853ce7f6
https://doi.org/10.5194/se-2020-95

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Paleozoic subduction of the southern Dunhuang Orogenic Belt, northwest China: metamorphism and geochronology of the Shuixiakou area

Autor: Chun-Ming Wu, Qian W.L. Zhang, Van Tho Pham, Hong-Xu Chen, Jia-Hui Liu, Tao Peng, Hao Y.C. Wang, Hui C.G. Zhang

Publikováno v: Geodinamica Acta, Vol 30, Iss 1, Pp 63-83 (2018)

Amphibolites in the Shuixiakou area of the southern Dunhuang Orogenic Belt, southernmost Central Asian Orogenic Belt (CAOB), occur as lenses within hornblende-biotite-plagioclase gneiss or pelitic schist, exhibiting block-in-matrix feature of tectoni

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::9d8c3cb5e4cc8d7e063a92aa3479ffb8
https://doaj.org/article/dd42bec7633a40e6808ca114d4dd8d56

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