Zobrazeno 1 - 10
of 16
pro vyhledávání: '"Valentina Taranovic"'
Autor:
Louise Schoneveld, Stephen J. Barnes, Hannu V. Makkonen, Margaux Le Vaillant, David J. Paterson, Valentina Taranovic, Kai-Yuan Wang, Ya-Jing Mao
Publikováno v:
Frontiers in Earth Science, Vol 8 (2020)
Small intrusions dominated by olivine- and pyroxene-rich cumulates are well known to be favorable hosts to magmatic Ni-Cu-(Platinum Group Element—PGE) sulfide mineralization. Such intrusions are common in a variety of settings around the world, but
Externí odkaz:
https://doaj.org/article/5f5970da31774ae3976573bc4d0ca947
Autor:
Stephen J. Barnes, Zhuo-Sen Yao, Ya-Jing Mao, Ana P. Jesus, Shenghong Yang, Valentina Taranovic, Wolfgang D. Maier
Publikováno v:
American Mineralogist. 108:1-17
Nickel contents of olivine have been widely used as petrogenetic indicators and as fertility indicators for magmatic sulfide potential of mafic-ultramafic intrusions, on the assumption that olivines crystallized from magmas that had equilibrated with
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::52b082f2c385d6c3baa4982cc1640f68
https://doi.org/10.2138/am-2022-8327
https://doi.org/10.2138/am-2022-8327
Publikováno v:
Economic Geology. 117:1687-1707
The Nova-Bollinger Ni-Cu-platinum group element (PGE) deposit in the Fraser zone of the Albany-Fraser orogen consists of two main orebodies, Nova and Bollinger, hosted by the same tube-shaped intrusion but having distinctly different Ni tenors of aro
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0843d19a9c1779542864e7bc4c9d0628
https://doi.org/10.5382/econgeo.4894
https://doi.org/10.5382/econgeo.4894
Autor:
Colin M. MacRae, Steve Beresford, Valentina Taranovic, Louise Schoneveld, Stephen Barnes, Morgan Williams
Publikováno v:
Economic Geology. 117:455-484
The Nova-Bollinger Ni-Cu sulfide ore deposit is the first economic Ni-Cu-Co sulfide deposit to have been discovered in the Albany-Fraser orogen in Western Australia. The host rocks are mafic-ultramafic intrusive cumulates subdivided into two connecte
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d9cb4866380ec3a553607b1e0edbd8ab
https://doi.org/10.5382/econgeo.4873
https://doi.org/10.5382/econgeo.4873
Publikováno v:
Economic Geology. 115:1749-1776
The Nova-Bollinger Ni-Cu sulfide deposit is associated with a small chonolith (tube-shaped) intrusion emplaced at lower crustal depths into granulite facies migmatite gneisses. The deposit comprises disseminated and net-textured ores within the intru
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::15a307b0ea1aa78a68ef52636175747a
https://doi.org/10.5382/econgeo.4758
https://doi.org/10.5382/econgeo.4758
Autor:
Mark A. Pearce, Natalia Torres-Rodriguez, Louise Schoneveld, Stephen Barnes, Michael Verrall, Valentina Taranovic
Publikováno v:
Journal of Petrology. 62
A prominent feature of the cumulate rocks of the Nova intrusions is the presence of reaction coronas between olivine and plagioclase. A particular spatial arrangement of mineral textures, typical of olivine–plagioclase coronas in high-P troctolites
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ceddf7b6697d56d8f8ddfb7c1af83665
https://doi.org/10.1093/petrology/egab055
https://doi.org/10.1093/petrology/egab055
Publikováno v:
ASEG Extended Abstracts. 2019:1-4
Small conduit or chonolith style intrusions dominated by olivine- and pyroxene-rich cumulates are well known to be favourable hosts to magmatic Ni-Cu-(PGE) sulfide mineralization. In many cases, su...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ad27fd328a863eddc57b2d3d6dd25830
https://doi.org/10.1080/22020586.2019.12073095
https://doi.org/10.1080/22020586.2019.12073095
Publikováno v:
ASEG Extended Abstracts. 2019:1-6
The Nova-Bollinger Ni-Cu sulfide ore deposits are hosted within a suite of mafic-ultramafic intrusive cumulate bodies. The Lower Intrusion is a thin semi-conformable chonolith comprising unlayered ...
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::38ed11890c79614616c69451ad941166
https://doi.org/10.1080/22020586.2019.12073068
https://doi.org/10.1080/22020586.2019.12073068
Publikováno v:
Economic Geology. 113:1161-1179
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b164487b7b3b4821606c89345da19a5f
https://doi.org/10.5382/econgeo.2018.4585
https://doi.org/10.5382/econgeo.2018.4585
Publikováno v:
International Geology Review. 59:1276-1291
The Xinyuan intrusion of the Eastern Junggar terrane is one of the mafic–ultramafic intrusions located in the Northern Xinjiang region and is associated with the southern part of the Central Asian Orogenic Belt (CAOB). Based on the secondary ion ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1a16f71918345ed7dbf5b68e573e356a
https://doi.org/10.1080/00206814.2016.1209435
https://doi.org/10.1080/00206814.2016.1209435