Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Hong‐Kun Dai"'
Autor:
Qing Xiong, Hong-Kun Dai, Jian-Ping Zheng, William L. Griffin, Hong-Da Zheng, Li Wang, Suzanne Y. O’ Reilly
Publikováno v:
Nature Communications, Vol 13, Iss 1, Pp 1-11 (2022)
Upward depletion of ophiolitic mantle is produced by melt-peridotite reaction with lateral melt/rock ratio variations in an asthenospheric upwelling column, which flows to become the horizontal oceanic lithospheric mantle under spreading centers.
Externí odkaz:
https://doaj.org/article/cb7fa912541e4b0a9826f3fe3428c641
Publikováno v:
Geophysical Research Letters, Vol 50, Iss 17, Pp n/a-n/a (2023)
Abstract A diffuse magmatic province covering central‐eastern Asia continent displays a compositional transition at 120–100 Ma and probably reflects melting initiation in isotopically enriched lithospheric mantle, followed by melting of the asthe
Externí odkaz:
https://doaj.org/article/737b296c27044bfaaf56ffbbb7eef267
Autor:
Hong-Kun Dai, Jian-Ping Zheng
Publikováno v:
Solid Earth Sciences, Vol 4, Iss 4, Pp 150-158 (2019)
Oceanic subduction is an important trigger for mantle heterogeneity, which further increases melt production and controls the compositions of intraplate basalts. Such a role played by the (Paleo-) Pacific subduction have been extensively studied and
Externí odkaz:
https://doaj.org/article/5c63e0b379bf42acad64643212982bcf
Autor:
Fabin Pan, Hongfei Zhang, Xiaobo He, Nigel Harris, Hong-Kun Dai, Qing Xiong, Biji Luo, Dong Liu, Timothy Kusky, Izhar Sadiq
Publikováno v:
Geological Society of America Bulletin.
The distribution of Oligo−Miocene magmatic rocks from southern Tibet in space and time yields critical information on the geometry and deformation of the subducted Indian lithosphere which impacts on plateau growth following the India and Eurasia c
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3b19a9ca57a2ac1b729d61a04ce7bb99
https://doi.org/10.1130/b36746.1
https://doi.org/10.1130/b36746.1
Autor:
Liang Zhou, Yu-Ping Su, Jian-Ping Zheng, Hong-Kun Dai, Qiang Ma, Jian Wang, Sai Zhang, Xia-Hui Zhang, Kai Xiong
Publikováno v:
Chemical Geology. 632:121537
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::7f1e577f1cc014e7cd3950ecda4944dd
https://doi.org/10.1016/j.chemgeo.2023.121537
https://doi.org/10.1016/j.chemgeo.2023.121537
Autor:
Jiang-Gu Lu, William L. Griffin, Jin-Xiang Huang, Hong-Kun Dai, Montgarri Castillo-Oliver, Suzanne Y. O’Reilly
Publikováno v:
Contributions to Mineralogy and Petrology. 177
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e92f350e082a47406b7d86ccc75ac032
https://doi.org/10.1007/s00410-022-01897-7
https://doi.org/10.1007/s00410-022-01897-7
Autor:
Xiang Zhou, Jian-Ping Zheng, Zeng-Bao Huang, Zhi-Yong Li, Wei-Qi Zhang, Hong-Da Zheng, Qing Xiong, Hong-Kun Dai
Publikováno v:
Lithos. :106985
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::537ff0f45c5c7fbd301c0d894d3d09cc
https://doi.org/10.1016/j.lithos.2022.106985
https://doi.org/10.1016/j.lithos.2022.106985
Autor:
Jian-Ping Zheng, Hong-Kun Dai
Publikováno v:
Solid Earth Sciences, Vol 4, Iss 4, Pp 150-158 (2019)
Oceanic subduction is an important trigger for mantle heterogeneity, which further increases melt production and controls the compositions of intraplate basalts. Such a role played by the (Paleo-) Pacific subduction have been extensively studied and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cab2d7873380d7000f55e250abd2387c
https://doi.org/10.1016/j.sesci.2019.09.001
https://doi.org/10.1016/j.sesci.2019.09.001
Publikováno v:
Lithos. :106623
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::19effb0015bdc9475741f08463b66c72
https://doi.org/10.1016/j.lithos.2022.106623
https://doi.org/10.1016/j.lithos.2022.106623
Publikováno v:
Lithos. :222-231
The geochemical signatures (i.e., high Sr/Y and La/Yb ratios) of adakitic rocks in continental settings, which are derived from the continental lower crust rather than from subducted slabs, may reflect high-pressure melting in the lower crust or may
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6cd1ac2cdc9b6cc175b37643adcf8b56
https://doi.org/10.1016/j.lithos.2016.12.020
https://doi.org/10.1016/j.lithos.2016.12.020