Zobrazeno 1 - 10
of 34
pro vyhledávání: '"Jens C.Ø. Andersen"'
Autor:
Reimar Seltmann, Jens C.Ø. Andersen, Chunji Xue, Xiaobo Zhao, Ling Xing, Xinjie Cui, Weice Zhao, Alla Dolgopolova
Publikováno v:
Geological Society, London, Special Publications. 516:155-176
The western Tianshan Gold Belt hosts numerous giant and large gold deposits that have been formed during the late Paleozoic amalgamation of the Tianshan orogen. However, little is known about their exhumation histories during the Mesozoic to Cenozoic
The skarns at Gryll’s Bunny are dominated by garnet and magnetite with small amounts of hornblende, epidote, apatite and tourmaline. They formed discordantly within a succession of metabasalts and metapelites (the Mylor Slate formation) within the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b7c772751fc5fe1c8bce8bb0fc047214
https://doi.org/10.5194/egusphere-egu22-4200
https://doi.org/10.5194/egusphere-egu22-4200
Autor:
Xiaobo Zhao, Reimar Seltmann, Chunji Xue, Alla Dolgopolova, Guozhen Zhang, Jens C.Ø. Andersen
Publikováno v:
Geological Journal. 55:2318-2341
Autor:
Jens C.Ø. Andersen, Iain McDonald, Marcell L. Besser, Jordan James Lindsay, Otavio Augusto Boni Licht, Hannah S.R. Hughes, Alan R. Hastie, Edir Edemir Arioli
The 135 Ma Parana-Etendeka Large Igneous Province (PELIP) is one of the largest areas of continental flood basalt (CFB) volcanism in the world and is widely agreed to be a product of intracontinental melts related to thermal anomalies from the Trista
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7748ab1a1f1511a024e8be8aed954f32
https://orca.cardiff.ac.uk/id/eprint/143628/1/1-s2.0-S0016703721004531-main.pdf
https://orca.cardiff.ac.uk/id/eprint/143628/1/1-s2.0-S0016703721004531-main.pdf
Autor:
Hannah S.R. Hughes, Jordan James Lindsay, Jens C.Ø. Andersen, Iain McDonald, Christopher M. Yeomans
Publikováno v:
Earth Science, Systems and Society. 1
Large Igneous Provinces, and by extension the mantle plumes that generate them, are frequently associated with platinum-group element (PGE) ore deposits, yet the processes controlling the metal budget in plume-derived magmas remains debated. In this
Autor:
Jens C.Ø. Andersen, S M Weatherley, Troels F.D. Nielsen, N. S. Rudashevsky, V. N. Rudashevsky
Publikováno v:
Journal of Petrology. 60:1903-1934
The Skaergaard PGE–Au mineralization, aka the Platinova Reef, is a syn-magmatic Platinum Group Element (PGE) and gold (Au) mineralization that formed after crystallization of ∼74% of the bulk melt of the intrusion. It is hosted in a more than 600
Autor:
Dermot Smyth, Iain McDonald, Jordan James Lindsay, Jens C.Ø. Andersen, Adrian J. Boyce, Hannah S.R. Hughes
Publikováno v:
Canadian Journal of Earth Sciences. 56:774-789
The ∼60 m thick Magilligan Sill is part of the British Palaeogene Igneous Province in the North Atlantic. The sill comprises layers of dolerite and olivine gabbro, and it intrudes a thick sequence of Mesozoic mudstones and marls, which are locally
Autor:
Christopher M. Yeomans, Hannah S.R. Hughes, Iain McDonald, Jordan James Lindsay, Jens C.Ø. Andersen
Publikováno v:
Geoscience Frontiers, Vol 12, Iss 3, Pp 101098-(2021)
Whilst traditional approaches to geochemistry provide valuable insights into magmatic processes such as melting and element fractionation, by considering entire regional data sets on an objective basis using machine learning algorithms (MLAs), we can
Publikováno v:
Lithos
The pre-Himalayan peraluminous magmatic event along the northern margin of Indian plate in north-western Pakistan has been investigated leading to a correlation with the magmatic evolution in other Himalayan and northern Gondwana regions. The two mic
Autor:
Miao Yu, Daxin Li, Chengyou Feng, Reimar Seltmann, Jens C.Ø. Andersen, Alla Dolgopolova, Shihua Zhong
Publikováno v:
Ore Geology Reviews. 93:19-37
The Weibao Cu-Pb-Zn deposit is typical of skarn deposits in the Qimantagh metallogenic belt (QMB), East Kunlun Mountains, northern Tibetan Plateau. It comprises three ore blocks from west to east, known as Weixi, Main and Weidong. Mineralization in t