Zobrazeno 1 - 10
of 17
pro vyhledávání: '"Qunzi Jia"'
Autor:
Jinchao Li, Yijie Gao, Yuegao Liu, Wei Wang, Huilei Kong, Xuegang Yao, Xiaobing Song, Qunzi Jia, Yazhi Li, Namkha Norbu, Xianzheng Guo
Publikováno v:
Geosciences Journal. 25:763-786
The East Kunlun orogenic belt (EKOB) is located in the northeastern part of the Qinghai-Tibetan Plateau, China. Voluminous Silurian-Devonian granitoids were formed during the Proto-Tethys Ocean subduction and collision process. In this study, zircon
Publikováno v:
Minerals; Volume 13; Issue 1; Pages: 74
The East Kunlun Orogenic Belt is considered as one of the important gold mineralization regions in the Tethys tectonic domain. These orogenic gold deposits are related to intermediate-acid intrusions formed at the end of Paleo-Tethys evolution, but t
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
Publikováno v:
Ore Geology Reviews. 145:104891
Publikováno v:
Minerals
Volume 10
Issue 11
Minerals, Vol 10, Iss 950, p 950 (2020)
Volume 10
Issue 11
Minerals, Vol 10, Iss 950, p 950 (2020)
The Gayahedonggou magmatic Cu-Ni sulfide deposit was recently discovered in the East Kunlun orogenic belt (Northern Tibetan Plateau, China). The mineralization in this region is associated with mafic&ndash
ultramafic intrusions. To date, the for
ultramafic intrusions. To date, the for
Autor:
YueGao Liu, ZhiBing Zhang, ZhaoWei Zhang, ZhiAn Wang, JiangWei Zhang, QunZi Jia, Bing Qian, WenYuan Li
Publikováno v:
Economic Geology. 113:1383-1417
Publikováno v:
Ore Geology Reviews. 118:103370
Abundant granitoids are exposed along the East Kunlun orogenic belt (EKOB), and many skarn deposits occur at the contacts between intrusions and strata. One such is the Xiaowolong deposit, a skarn-type tin polymetallic deposit that is temporally and
Publikováno v:
Minerals
Volume 9
Issue 9
Minerals, Vol 9, Iss 9, p 547 (2019)
Volume 9
Issue 9
Minerals, Vol 9, Iss 9, p 547 (2019)
The Reshui porphyry Mo deposit is located in the East Kunlun orogenic belt (EKOB). Molybdenum mineralization is distributed in monzogranite and porphyritic monzogranite rocks, mainly presenting as various types of hydrothermal veinlets in altered wal
Autor:
Norbu, Namkha1 (AUTHOR), Tang, Ling2 (AUTHOR) tangling@ieecas.cn, Li, Jinchao3 (AUTHOR) tangling@ieecas.cn, Kong, Huilei3 (AUTHOR), Li, Yazhi3 (AUTHOR), Jia, Qunzi3 (AUTHOR), Xu, Yan1 (AUTHOR)
Publikováno v:
Minerals (2075-163X). Jan2023, Vol. 13 Issue 1, p74. 20p.
Publikováno v:
Geological Journal; May2022, Vol. 57 Issue 5, p1759-1782, 24p