Zobrazeno 1 - 10
of 111
pro vyhledávání: '"Juxing TANG"'
Autor:
Faqiao Li, Juxing Tang, Yang Song, She Li, Pan Tang, Haifeng Li, Huanhuan Yang, Qin Wang, Yongqiang Wang, Zongzhui Danzeng, Yanbo Li, Jianli Li, Hongwei Li, Yujie Dong
Publikováno v:
Frontiers in Earth Science, Vol 12 (2024)
Chlorite is present extensively in many types of deposits. The mechanism underlying the chemical variations in chlorite remains unclear. The Naruo porphyry deposit is a giant copper porphyry deposit in the Duolong ore district of Tibet. Chlorite, whi
Externí odkaz:
https://doaj.org/article/6e908fc73b3745d3a8c557959fd8ef16
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
The Bangong–Nujiang metallogenic belt consists of scattered Tethyan oceanic blocks, mainly distributed underneath the margins of the Qiangtang and Lhasa terranes in central Tibet. A new world-class metallogenic belt has been reported in this region
Externí odkaz:
https://doaj.org/article/5d343180a763496aa74b2c939b371611
Autor:
Zongyao Yang, Juxing Tang, M. Santosh, Xiaoyan Zhao, Xinghai Lang, Ying Wang, Shuai Ding, Fengqin Ran
Publikováno v:
Scientific Reports, Vol 11, Iss 1, Pp 1-13 (2021)
Abstract Continental crust has long been considered too buoyant to be subducted beneath another continent, although geophysical evidence in collision zones predict continental crust subduction. This is particularly significant where upper continental
Externí odkaz:
https://doaj.org/article/8b9113dd092c4010bb0b3df877d982d8
Autor:
Tingbin Zhang, Guihua Yi, Hongmei Li, Ziyi Wang, Juxing Tang, Kanghui Zhong, Yubin Li, Qin Wang, Xiaojuan Bie
Publikováno v:
Remote Sensing, Vol 8, Iss 11, p 890 (2016)
One of the most important characteristics of porphyry copper deposits (PCDs) is the type and distribution pattern of alteration zones which can be used for screening and recognizing these deposits. Hydrothermal alteration minerals with diagnostic spe
Externí odkaz:
https://doaj.org/article/4c7fb0201fd04ac0990558866abf0785
Autor:
Xiaoxu, Zhang, Juxing, Tang, Bin, Lin, Qin, Wang, Liang, He, Gang, Yan, Rui, Shao, Qiang, Wu, Qiu, Du, Pingcuo, Zhaxi
Publikováno v:
In Ore Geology Reviews March 2023 154
Publikováno v:
Geological Magazine. :1-16
The subduction of the Bangong–Nujiang Ocean is important in the geological evolution of the Tibetan Plateau. In this paper, we report new zircon U-Pb age and Lu-Hf isotopic data and whole-rock elemental and Sr-Nd-Pb isotopic data for Early Cretaceo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::3b5f7bfaf53e8608f44b1af5cf4bb0a2
https://doi.org/10.1017/s0016756823000274
https://doi.org/10.1017/s0016756823000274
Publikováno v:
Journal of Earth Science. 34:467-486
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c69c87a156e269bb87867cca9238681a
https://doi.org/10.1007/s12583-020-1076-5
https://doi.org/10.1007/s12583-020-1076-5
Autor:
Faqiao LI, Juxing TANG, Nan WANG, Zhibo LIU, Yang SONG, Jing ZHANG, Xudong MA, Bin FU, Haifeng LI, Songhao HAN
Publikováno v:
Acta Geologica Sinica - English Edition. 96:1960-1978
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::fe03272dfd8cee114dedb44a9daf5cc0
https://doi.org/10.1111/1755-6724.14936
https://doi.org/10.1111/1755-6724.14936
Autor:
Xiaoxu ZHANG, Bin LIN, Juxing TANG, Liang HE, Zhibo LIU, Qin WANG, Rui SHAO, Qiu DU, Wangdui SILANG, Ouzhu CIREN, Quzhen GUSANG, Zhongga CIDAN
Publikováno v:
Acta Geologica Sinica - English Edition. 96:1221-1236
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d216a34f63952699c52ee9acf663fd07
https://doi.org/10.1111/1755-6724.14807
https://doi.org/10.1111/1755-6724.14807
Autor:
Tao, Pan Tang, Juxing Tang, Xinghai Lang, Bin Lin, Fuwei Xie, Miao Sun, Faqiao Li, Jing Qi, Hao Cui, Mengdie Wang, Yan Xiong, Gang
Publikováno v:
Minerals; Volume 13; Issue 7; Pages: 876
The Xiongcun Cu–Au ore district is in the southern middle Gangdese Metallogenic Belt, Tibet, and formed during Neo-Tethyan oceanic subduction. The Xiongcun ore district mainly comprises two deposits, the No. I and No. II deposits, which were formed
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=multidiscipl::0953410003145f36e81996fbf801f7bb