Zobrazeno 1 - 10 of 82 pro vyhledávání: '"Bao Fu Han"'
3
Trench retreat recorded by a subduction zone metamorphic history
Autor: Jie Dong, Marty Grove, Chunjing Wei, Bao-Fu Han, An Yin, Jiafu Chen, Ang Li, Zhicheng Zhang
Publikováno v: Geology. 50:1281-1286
Upper amphibolite-facies metamorphism in subduction zone rocks may occur under exceptional tectonic settings. Differentiating competing mechanisms for its occurrence requires carefully integrated, high-resolution thermobarometric and geochronologic s
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::1ecba9e8cc6e607abba5f06ade92e4ba
https://doi.org/10.1130/g50385.1
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4
Ages and tectonic attributes of Late Palaeozoic stratigraphic units in the Tarbagatay, West Junggar (NW China): revisited
Autor: Yan Xu, Bao-Fu Han, Ang Li, Wen Liao
Publikováno v: International Geology Review. 64:2766-2782
As the youngest single age of detrital zircons is used as the maximum depositional age, the ages and tectonic attributes of the Late Palaeozoic stratigraphic units in the Tarbagatay area, West Jung...
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::30d4a903844a02c9f0504f15193e5e30
https://doi.org/10.1080/00206814.2021.2001697
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7
Ediacaran initial subduction and Cambrian slab rollback of the Junggar Ocean: New evidence from igneous tectonic blocks and gabbro enclave in Early Palaeozoic accretionary complexes, southern West Junggar, NW China
Autor: Bao-Fu Han, Ang Li, Wen Liao, Yan Xu
Publikováno v: Geological Magazine. 158:1811-1829
New zircon U–Pb ages and whole-rock chemical data from four adakitic and two non-adakitic igneous rocks as tectonic blocks in the southern West Junggar accretionary complexes, northwestern China and one gabbro enclave in adakitic block provide furt
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::952fbc66a8abef6b198faf2c28d8fe34
https://doi.org/10.1017/s0016756821000376
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8
Geochronological and geochemical evidence for a Late Ordovician to Silurian arc–back-arc system in the northern Great Xing’an Range, NE China
Autor: Bao-Fu Han, Junlai Liu, Jia-Fu Chen, Bo Liu, Jia-Wei Li
Publikováno v: Geoscience Frontiers, Vol 12, Iss 1, Pp 131-145 (2021)
The early Paleozoic tectonic evolution of the Xing’an–Mongolian Orogenic Belt is dominated by two oceanic basins on the northwestern and southeastern sides of the Xing’an Block, i.e., the Xinlin–Xiguitu Ocean and the Nenjiang Ocean. However,
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::b0c76d064113a5de829c56eba4c51c0a
https://doi.org/10.1016/j.gsf.2020.07.002
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9
Multiphase Late Devonian to Carboniferous volcanic events in the west of Oyu Tolgoi, southeastern Mongolia: New geochronological, geochemical, and isotopic constraints on tectonic history
Autor: Bao-Fu Han, Narantsetseg Tserendash, Zejia Ji, Zhicheng Zhang
Publikováno v: Gondwana Research. 88:169-184
The Late Paleozoic volcanic rocks distributed in southeastern Mongolia are key to reconstructing the tectonic processes along the south margin of the Central Asian Orogenic Belt during this period. In this study, representative volcanic samples were
Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_________::a073968cf8297b0ba85a9737f4e92061
https://doi.org/10.1016/j.gr.2020.08.008
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