Zobrazeno 1 - 10
of 40
pro vyhledávání: '"Qihai Shu"'
Autor:
Fan Yu, Qihai Shu, Xudong Niu, Kai Xing, Linlong Li, David R. Lentz, Qingwen Zeng, Wenjie Yang
Publikováno v:
Minerals, Vol 10, Iss 5, p 456 (2020)
The Xianghualing skarn Sn deposit in the southwestern part of the southern Hunan Metallogenic Belt is a large Sn deposit in the Nanling area. In this paper, the garnet has been analyzed by laser ablation-inductively coupled plasma-mass spectrometry (
Externí odkaz:
https://doaj.org/article/f4c46cc015ec49d3beecd4932735b37c
Publikováno v:
Geofluids, Vol 2017 (2017)
The Haisugou porphyry Mo deposit is located in the northern Xilamulun district, northeastern China. Based on alteration and mineralization styles and crosscutting relationships, the hydrothermal evolution in Haisugou can be divided into three stages:
Externí odkaz:
https://doaj.org/article/ea65ad7aa18b443d9fc3d65a37392cb4
Publikováno v:
Economic Geology. 118:485-507
The timescales and duration of ore-forming processes in skarn systems are not well constrained. To better understand this, we present high-precision chemical abrasion-isotope dilution-thermal ionization mass spectrometry (CA-ID-TIMS) U-Pb zircon and
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f21a053079f21ba33b7609021162e4c2
https://doi.org/10.5382/econgeo.4984
https://doi.org/10.5382/econgeo.4984
Publikováno v:
Acta Geochimica. 41:185-196
The Baiyinnuo’er deposit in northern China is located in the south section of the Great Xing’an Range, and it is the largest skarn Zn–Pb deposit in the region. Skarn and Zn–Pb orebodies mainly occur between the different units of the Permian
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::bbf0b1c26b640cb8c8f07092123255b2
https://doi.org/10.1007/s11631-021-00504-z
https://doi.org/10.1007/s11631-021-00504-z
Publikováno v:
Geology. 49:473-477
Fluid inclusion compositions obtained from laser ablation–inductively coupled plasma–mass spectrometry at the Haobugao Zn-Pb skarn in northeastern China provide constraints on fluid origin, evolution, and metal deposition mechanisms and an exampl
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::39ff36279643fe6ad2cfd11d14b3ac97
https://doi.org/10.1130/g48348.1
https://doi.org/10.1130/g48348.1
Autor:
Jun Deng, Qingfei Wang, Xiang Sun, Lin Yang, David I. Groves, Qihai Shu, Liang Gao, Liqiang Yang, Kunfeng Qiu, Changming Wang, Chaoyi Dong
Publikováno v:
Earth-Science Reviews. 235:104245
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a3957ba008d9bc78b7f02f48f17ca3ea
https://doi.org/10.1016/j.earscirev.2022.104245
https://doi.org/10.1016/j.earscirev.2022.104245
Publikováno v:
Gondwana Research. 73:65-76
Although garnet U Pb dating method has been reported recently, yet the accurate concordia 206Pb/238U ages and growth histories of multi generation of garnets based on ages were still lacked. LA-ICP-MS U Pb dating on multi-generational grandite (gross
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c1872996582c542ee4cc18ad2e0c345d
https://doi.org/10.1016/j.gr.2019.04.003
https://doi.org/10.1016/j.gr.2019.04.003
Autor:
Huaying Wu, Yong Zhang, Xinlu Hu, Pin Wang, Cheng Zhang, Yong Lai, Qihai Shu, Degao Zhai, Zhaoshan Chang
Publikováno v:
Mineralium Deposita. 54:645-656
It has been widely accepted that magmas genetically linked to porphyry (-skarn) Cu (Mo) deposits are commonly oxidized. Recently, using laser ablation-inductively coupled plasma-mass spectrometry (LA-ICP-MS) techniques, zircon Ce4+/Ce3+, CeN/CeN*, Eu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2df2f1159a968f5a7dce159859b1f807
https://doi.org/10.1007/s00126-019-00867-7
https://doi.org/10.1007/s00126-019-00867-7
Publikováno v:
Geoscience Frontiers. 13:101401
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::36e00e964b2bae2aa4030cd777c1e57e
https://doi.org/10.1016/j.gsf.2022.101401
https://doi.org/10.1016/j.gsf.2022.101401
Publikováno v:
Ore Geology Reviews. 145:104877
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2ded7935adbf969bf92dc2582483794f
https://doi.org/10.1016/j.oregeorev.2022.104877
https://doi.org/10.1016/j.oregeorev.2022.104877