Zobrazeno 1 - 3
of 3
pro vyhledávání: '"Min-xin You"'
Autor:
Zhao-wei Zhang, Ya-lei Wang, Chi-yuan Wang, Bing Qian, Wen-yuan Li, Jiang-wei Zhang, Min-xin You
Publikováno v:
China Geology, Vol 2, Iss 4, Pp 467-477 (2019)
ABSTRACT: The Eastern Kunlun Orogenic Belt (EKOB) has a complex geological structure and diverse magmatic activities, which are closely related to the Qaidam Basin and the Tethys tectonic evolution. There are at least 3 stages mafic-ultramafic rocks
Externí odkaz:
https://doaj.org/article/80c18fa8fb43405d95b260a32732b162
Autor:
Wen-yuan Li, Fang Liu, Zhao-wei Zhang, Ya-lei Wang, XunHui Xu, Min-xin You, Xin Kou, YueGao Liu, ZhengGuo Chen, QunZi Jia
Publikováno v:
Journal of Geochemical Exploration. 198:41-53
The East Kunlun Orogenic Belt experienced two periods of mantle-derived magmatic activity during its post-collisional stages. One occurred during the Late Silurian-Early Devonian, and the other occurred during the Middle-Late Triassic. The Late Silur
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1a6cef823c4cf8e8ad3031aa78e21fb5
https://doi.org/10.1016/j.gexplo.2018.12.002
https://doi.org/10.1016/j.gexplo.2018.12.002
Publikováno v:
Minerals, Vol 11, Iss 348, p 348 (2021)
Minerals
Volume 11
Issue 4
Minerals
Volume 11
Issue 4
The Baixintan mafic-ultramafic intrusion in the Dananhu-Tousuquan arc of the Eastern Tianshan orogenic belt is composed of lherzolite, olivine gabbro, and gabbro. Olivine gabbros contain zircon grains with a U-Pb age of 276.8 ± 1.1 Ma, similar to th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::c5bedbc572f9529e5922e07264f59ec9
https://doi.org/10.3390/min11040348
https://doi.org/10.3390/min11040348