Zobrazeno 1 - 8
of 8
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0e6f6c429987b582608daacdeda54d02
https://doi.org/10.1007/s12303-021-0017-3
https://doi.org/10.1007/s12303-021-0017-3
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a6fd6c4fbf371869be56f320c34f18d6
https://doi.org/10.3390/min13010074
https://doi.org/10.3390/min13010074
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:
Ore Geology Reviews. 145:104891
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bba0c14fec2e7792750fd9c286feced3
https://doi.org/10.1016/j.oregeorev.2022.104891
https://doi.org/10.1016/j.oregeorev.2022.104891
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f5108154abc83645f7767879dbdfe9a2
Autor:
YueGao Liu, ZhiBing Zhang, ZhaoWei Zhang, ZhiAn Wang, JiangWei Zhang, QunZi Jia, Bing Qian, WenYuan Li
Publikováno v:
Economic Geology. 113:1383-1417
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::392f74446235ac4a893d9f9540e68c20
https://doi.org/10.5382/econgeo.2018.4596
https://doi.org/10.5382/econgeo.2018.4596
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::058c3a7d8e0f618c8fc0563ad46af4d0
https://doi.org/10.1016/j.oregeorev.2020.103370
https://doi.org/10.1016/j.oregeorev.2020.103370
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
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d6e01dc55f802c7159be86f1a34d301a
https://doi.org/10.3390/min9090547
https://doi.org/10.3390/min9090547