Zobrazeno 1 - 10
of 73
pro vyhledávání: '"Xuexiang, GU"'
Publikováno v:
In Ore Geology Reviews May 2023 156
Publikováno v:
Acta Geologica Sinica - English Edition. 97:404-417
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ea3d2118b097c25e179a4ba2494f889f
https://doi.org/10.1111/1755-6724.14964
https://doi.org/10.1111/1755-6724.14964
Publikováno v:
Earth Sciences Research Journal, Vol 22, Iss 4, Pp 301-318 (2018)
The Gaosongshan epithermal gold deposit in Heilongjiang, Northeast China, is hosted by the Lower Cretaceous intermediate-basic volcanic rocks. Three auriferous quartz veins including eleven gold orebodies were all discovered in tectonoclastic zones.
Externí odkaz:
https://doaj.org/article/047e4fee199b4a5c81d1cee6a3a3ae10
Publikováno v:
Geological Society of America Bulletin. Jan/Feb2024, Vol. 136 Issue 1/2, p461-486. 26p.
There are many lode gold deposits and occurrences in the Kalamaili area of the East Junggar, Northwestern China. The deposits are confined to a narrow zone between the regional NW- to NWW-trending Kalamaili and Qingshui-Sujiquan shear zones and are s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::741c3ca1192df7c624d0b4464f95bcf4
https://doi.org/10.5194/egusphere-egu23-3845
https://doi.org/10.5194/egusphere-egu23-3845
The Gaogangshan deposit in the northern Lesser Xing'an Range, NE China, consists of typical collision-type porphyry Mo mineralization related to Permo-Triassic granitic intrusions. Ore-forming process is recorded by multiple generations of quartz, in
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::2f75ba9065c96f1aecc708e6483fae44
https://doi.org/10.5194/egusphere-egu23-3809
https://doi.org/10.5194/egusphere-egu23-3809
Publikováno v:
GSA Bulletin.
There are many lode gold deposits and occurrences in the Kalamaili area of the East Junggar, northwestern China. However, little is known about the specifics of ore geology and geochemistry of these gold deposits because of very limited exploration a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::61aa4dce5046ca025fb0cff8e90de39f
https://doi.org/10.1130/b36650.1
https://doi.org/10.1130/b36650.1
Autor:
null et al., Xuexiang Gu
Figure S1: Field photographs of regional deformation. Figure S2: Jinshuiquan fluid inclusions. Figure S3: Nanmingshui fluid inclusions. Figure S4: Sujiquandong fluid inclusions. Table S1: Concentrations of Trace Elements in Quartz from the Gold Depos
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::0364fb029142b7e60a33813940068d0e
https://doi.org/10.1130/gsab.s.21919395.v1
https://doi.org/10.1130/gsab.s.21919395.v1
Publikováno v:
Journal of Petrology. 63
Scanning electron microscope, cathodoluminescence (CL) imaging and laser ablation–inductively coupled plasma–mass spectrometry analyses were conducted on coexisting pairs of quartz and K-feldspar from 14 samples of various types of felsic igneous
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::31c0620af800b41b55c6283cd7664309
https://doi.org/10.1093/petrology/egac113
https://doi.org/10.1093/petrology/egac113
Publikováno v:
Geological Journal. 56:2799-2815
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::517e1d2774a93ad0858193b104c421b8
https://doi.org/10.1002/gj.4070
https://doi.org/10.1002/gj.4070