Zobrazeno 1 - 10
of 19
pro vyhledávání: '"Jinhan Gao"'
Publikováno v:
Scientific Reports, Vol 12, Iss 1, Pp 1-12 (2022)
Abstract The Jurassic sequences in the South Qiangtang Basin of Tibet are essential for understanding the paleogeography and tectonic evolution of this basin and the Bangong-Nujiang Meso-Tethys Ocean (BNMO). However, the partial absence of fossils hi
Externí odkaz:
https://doaj.org/article/a3c5519a2a01412b994450c301f93d37
Autor:
Yaxi Wang, Xiao Liang, Genhou Wang, Jia Zhao, Jinhan Gao, Byung‐Su Lee, Yilong Zheng, Soo-In Park, Guo-Li Yuan, Qiang Fang, Dian Li, Haishui Jiang, Wentao Cao
Publikováno v:
Basin Research. 33:2383-2410
[The late Permian–Triassic trench‐slope basin in the CQMB showing the correlation between spatiotemporal variations in basin sedimentation and the extensional tectonism of the accretionary wedge. , Abstract Records of sedimentation and deformatio
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::286091ba589272c04360125cb0ae24a3
https://doi.org/10.1111/bre.12561
https://doi.org/10.1111/bre.12561
Publikováno v:
Geological Journal. 55:6625-6641
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::10ad5a85dd4f7f80439907f51c41a748
https://doi.org/10.1002/gj.3832
https://doi.org/10.1002/gj.3832
Publikováno v:
Tectonics. 39
Our field work was supported by the Young Scientist Fund of the National Natural Science Foundation of China (Grant 41402177). The experimental items were financially supported by the China Geological Survey (CGS): “1:50,000 regional geological sur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2d7691521804b71229cddba4a0fb0302
https://doi.org/10.1029/2019tc005589
https://doi.org/10.1029/2019tc005589
Publikováno v:
Journal of Asian Earth Sciences. 146:114-133
Upper Triassic reef corals from the Riganpeicuo Formation in northern Tibet represent important scleractinian coral fauna that help explain the palaeobiogeography of the eastern Tethys region during the Late Triassic period. The corals were discovere
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a96d9ce48feb4b1ff976286740474163
https://doi.org/10.1016/j.jseaes.2017.05.006
https://doi.org/10.1016/j.jseaes.2017.05.006
Autor:
Dian Li, Li Zhang, Guo-Li Yuan, Jie Zhou, Haichao Zhao, Yidong Gong, Genhou Wang, Da-Ren Fang, Jinhan Gao
Models of in situ oceanic subduction and underthrusting is proposed to explain the formation and exhumation of the central Qiangtang mélange belt. Some studies have suggested that continental subduction occurred in central Qiangtang, but there is a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::162e34d1d5cc487bff339a6f5f72b841
Publikováno v:
15th International Congress of the Brazilian Geophysical Society & EXPOGEF, Rio de Janeiro, Brazil, 31 July-3 August 2017.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b765e0e57d09473ca33c8c7f83f87221
https://doi.org/10.1190/sbgf2017-323
https://doi.org/10.1190/sbgf2017-323
Publikováno v:
Acta Geologica Sinica - English Edition. 84:483-496
The Mesoproterozoic Wumishan Formation at the Jixian section in Tianjin is a set of more than 3000-m-thick stromatolitic carbonate succession. In this succession, several lithofacies units, that is, the subtidal stromatolitic biostrome, the thromboli
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f747392fb01018fcab262719c729764
https://doi.org/10.1111/j.1755-6724.2010.00149.x
https://doi.org/10.1111/j.1755-6724.2010.00149.x
Publikováno v:
Earth Science Frontiers. 16:207-218
The Precambrian carbonate rocks are commonly characteristic of stromatolitic carbonate succession. However, in the western segment of Yanshan area, the third member of the Mesoproterozoic Gaoyuzhuang Formation at the Qiangou section in Yanqing, Beiji
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9128ea1d19729365338c89f4acb9d3ea
https://doi.org/10.1016/s1872-5791(08)60108-6
https://doi.org/10.1016/s1872-5791(08)60108-6