Zobrazeno 1 - 10
of 14
pro vyhledávání: '"Banxiao Ruan"'
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
The Qiyishan deposit is a large-scale Rb polymetallic deposit in the Beishan orogen. However, there remain debates regarding its metallogenic age and tectonic setting. In addition, studies of Triassic tectono-magmatic events in the Beishan orogen are
Externí odkaz:
https://doaj.org/article/39f9d98e3cea43fa9fe751da77103d9e
Publikováno v:
Minerals; Volume 13; Issue 3; Pages: 450
The Huanggang deposit is the most important and largest skarn Fe–Sn polymetallic deposit in the Southern Great Xing’an Range of Northeast China. Cassiterite, magnetite, and other metal minerals are related to the garnets within skarn systems. The
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::189244a96c5f766ee010e6cc59e40ce6
Publikováno v:
Minerals
Volume 10
Issue 12
Minerals, Vol 10, Iss 1050, p 1050 (2020)
Volume 10
Issue 12
Minerals, Vol 10, Iss 1050, p 1050 (2020)
The mineral chemistry of chromite and silicate minerals in the Baixintan magmatic Ni-Cu sulfide deposit in the Northern Tianshan, southern Central Asian Orogenic Belt (CAOB) are reported here. Two types of chromite were identified in mafic-ultramafic
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e32395d51aa34b4d46fada39ada40675
Publikováno v:
Ore Geology Reviews. 139:104423
In recent decades, new breakthroughs in Ni prospecting have been made in the Beishan area, southern Central Asian Orogenic Belt, NW China—more vein-type sulfide mineralization with high Ni tenor has been discovered. Here, novel discussions on the p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ecc2116a34de1328dc0e7c2e6c70e662
https://doi.org/10.1016/j.oregeorev.2021.104423
https://doi.org/10.1016/j.oregeorev.2021.104423
Publikováno v:
Ore Geology Reviews. 138:104408
The newly discovered Huangtan Au-Cu deposit is located in the central Dananhu - Tousuquan arc of Eastern Tianshan, southern Central Asian Orogenic Belt (CAOB). It is the first Au-dominated volcanogenic massive sulfide (VMS) polymetallic deposit in th
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::46e3bdbcaa88f4ff7ff65d008e7b732b
https://doi.org/10.1016/j.oregeorev.2021.104408
https://doi.org/10.1016/j.oregeorev.2021.104408
Publikováno v:
Ore Geology Reviews. 91:419-431
The Poyi Cu-Ni deposit is hosted by the Early Permian Pobei mafic-ultramafic complex along the northern margin of the Tarim Plate. This series of multiple intrusions in the Poyi deposit can be divided into four lithologies: gabbro, dunite, hornblende
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::86530531fd02ed7a80521dbf8dc9728b
https://doi.org/10.1016/j.oregeorev.2017.09.013
https://doi.org/10.1016/j.oregeorev.2017.09.013
Publikováno v:
Mineralogy and Petrology. 111:693-708
The Hongshishan mafic-ultramafic complex is located in the western Beishan Terrane, NW China, and hosts an economic Ni-Cu deposit. Chromite as accessory mineral from the complex is divided into three types based on its occurrence and morphology. Quan
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b0d058ab643fed278354e0814abf1bd5
https://doi.org/10.1007/s00710-016-0480-0
https://doi.org/10.1007/s00710-016-0480-0
Publikováno v:
Resource Geology. 66:313-334
The Kuluketage block, located in the northeast Tarim craton, is one of the largest Precambrian blocks in the Xinjiang province. Recently, many banded iron formation (BIF)-type (Superior-type) deposits have been discovered in the western part of the K
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ce4d465ad7be67ae91f605c9dbb94e99
https://doi.org/10.1111/rge.12107
https://doi.org/10.1111/rge.12107
Autor:
Yanrong Liu, Xinbiao Lü, Banxiao Ruan, Jian Ma, Munir Mohammed Abdalla Adam, Yuegao Liu, Xiaofeng Cao
Publikováno v:
Journal of Asian Earth Sciences. 118:81-94
The Posan ultramafic intrusion is one of the ~280 Ma Pobei mafic–ultramafic complexes located in the Beishan rift, on the northeastern margin of the Tarim Craton. Given that three finished drill holes reveal less economic mineralization, it is nece
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eddc13d182290d33f237f209edb2c797
https://doi.org/10.1016/j.jseaes.2015.12.020
https://doi.org/10.1016/j.jseaes.2015.12.020
Publikováno v:
Lithos. :105594
The Huangtan Au Cu deposit is was recently discovered in the Kalatag district, Xinjiang, NW China. It is one of the few Early Paleozoic volcanic massive sulfide (VMS) deposits in the East Tianshan. The deposit is predominantly hosted by Early Paleozo
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9a7b0fd1bfda0f8ffb30445a4cd7c419
https://doi.org/10.1016/j.lithos.2020.105594
https://doi.org/10.1016/j.lithos.2020.105594