Zobrazeno 1 - 10
of 10
pro vyhledávání: '"Jiu-Long Zhou"'
Publikováno v:
Science Bulletin. 65:1880-1883
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::adec1ecb5b267e197880a5b008a3392b
https://doi.org/10.1016/j.scib.2020.07.025
https://doi.org/10.1016/j.scib.2020.07.025
Publikováno v:
Earth and Planetary Science Letters. 594:117736
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f520d94764c73115118dd95dbf4d8ab7
https://doi.org/10.1016/j.epsl.2022.117736
https://doi.org/10.1016/j.epsl.2022.117736
Publikováno v:
Geological Society of America Abstracts with Programs.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c2b2b3387b82e7a64b6fa1de8c7c0e95
https://doi.org/10.1130/abs/2020am-356655
https://doi.org/10.1130/abs/2020am-356655
Publikováno v:
Precambrian Research. 306:94-111
The Neoproterozoic Imorona-Itsindro Suite of central Madagascar represents one of the crucial petrological records of the supercontinent transformation from Rodinia into Gondwana, whereas its tectonic setting remains open to debate. Here newly report
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1ba610027522bc189fa791201b17fa59
https://doi.org/10.1016/j.precamres.2017.12.029
https://doi.org/10.1016/j.precamres.2017.12.029
Autor:
Shun Guo, Li-Guang Wu, Chuan Yang, Songbai Peng, Kai Lu, Jiu-Long Zhou, Hao Deng, Xian-Hua Li
Publikováno v:
Precambrian Research. 346:105787
The present Yangtze Block was proposed to be formed as a unified block in the Mesoproterozoic-Neoproterozoic transition, but the detailed timing and process are poorly constrained. Here we report integrated in situ U–Pb and Hf–O isotopic analyses
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d9d4f0b01b0c03e9665b484f36c7af3d
https://doi.org/10.1016/j.precamres.2020.105787
https://doi.org/10.1016/j.precamres.2020.105787
Autor:
Jiu-Long Zhou
Publikováno v:
Precambrian Research. 262:123-126
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::51286a2a101b150e69911e337cf6e70a
https://doi.org/10.1016/j.precamres.2014.12.020
https://doi.org/10.1016/j.precamres.2014.12.020
Publikováno v:
Journal of African Earth Sciences. 106:75-86
New geochronological and geochemical data are presented on Early Cambrian granites from the Ambatondrazaka area in east-central Madagascar. U–Pb zircon dating reveals that these granites were emplaced at ∼520 Ma within a post-collisional setting.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c5f5673478e3b42c2f3f075032735636
https://doi.org/10.1016/j.jafrearsci.2015.02.012
https://doi.org/10.1016/j.jafrearsci.2015.02.012
Publikováno v:
Precambrian Research. 256:256-270
Tectonic setting of the ca. 840–760 Ma Imorona-Itsindro Suite throughout central Madagascar is critical to understanding Madagascar-India correlation in pre-Gondwana time and the paleogeography of the rifting Rodinia. Here, we present new geochrono
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ebc1070afc7d9ccfae9f89eb1b0292bd
https://doi.org/10.1016/j.precamres.2014.11.005
https://doi.org/10.1016/j.precamres.2014.11.005
Publikováno v:
Lithos. :339-360
It is well recognized that various degrees of mantle-derived materials are incorporated in the formation of granite, and mantle-derived mafic melts are generally considered to mix with crustal felsic melt. Here, however, we provide an example of the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c4cde801cfdfdd870689f87ca68a970b
https://doi.org/10.1016/j.lithos.2014.09.023
https://doi.org/10.1016/j.lithos.2014.09.023
Publikováno v:
Geoscience Frontiers, Vol 3, Iss 5, Pp 717-728 (2012)
According to the metallogenic theory by transmagmatic fluid (TMF), one magmatic intrusion is a channel of ore-bearing fluids, but not their source. Therefore, it is possible to use TMF’s ability for injection into and for escaping from the magmatic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::62629817cc589ce393874c5a190a00ea
https://doi.org/10.1016/j.gsf.2012.02.001
https://doi.org/10.1016/j.gsf.2012.02.001