Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Oleg M. Grinev"'
Autor:
Ksenia V. Bestemianova, Oleg M. Grinev
Publikováno v:
Известия Томского политехнического университета: Инжиниринг георесурсов, Vol 332, Iss 9, Pp 210-222 (2021)
Relevance of the research is conditioned by a need to understand the formation model of studied ore deposits; this leads to development of scientifically valid prediction and estimation and, hence, expansion of available mineral resources (first of a
Externí odkaz:
https://doaj.org/article/ce3ef2fc909e4ac9a774db8754944827
Autor:
Anatoly M. Sazonov, Aleksei E. Romanovsky, Igor F. Gertner, Elena A. Zvyagina, Tatyana S. Krasnova, Oleg M. Grinev, Sergey A. Silyanov, Yurii V. Kolmakov
Publikováno v:
Minerals, Vol 11, Iss 4, p 354 (2021)
The gold and platinum-group elements (PGE) mineralization of the Guli and Kresty intrusions was formed in the process of polyphase magmatism of the central type during the Permian and Triassic age. It is suggested that native osmium and iridium cryst
Externí odkaz:
https://doaj.org/article/b31e1b4fdd824dbda41399cbfd9ac1ab
Publikováno v:
Geosfernye issledovaniya. :95-100
Autor:
Oleg M. Grinev, E. A. Zvyagina, Tatyana S. Krasnova, A.M. Sazonov, Aleksei E. Romanovsky, I. F. Gertner, Sergey A. Silyanov, Yurii V. Kolmakov
Publikováno v:
Minerals. 2021. Vol. 11, № 4. P. 354 (1-20)
Minerals
Volume 11
Issue 4
Minerals, Vol 11, Iss 354, p 354 (2021)
Minerals
Volume 11
Issue 4
Minerals, Vol 11, Iss 354, p 354 (2021)
The gold and platinum-group elements (PGE) mineralization of the Guli and Kresty intrusions was formed in the process of polyphase magmatism of the central type during the Permian and Triassic age. It is suggested that native osmium and iridium cryst
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::78690ae0bf4457335506e40f6025b4fb
https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000895287
https://vital.lib.tsu.ru/vital/access/manager/Repository/koha:000895287
Publikováno v:
Global and Planetary Change. 185:103097
Large Igneous Provinces (LIPs) are emerging as a significant driver of short duration climatic change including mass extinctions. Here we compare the record of LIPs against the timing of Devonian biotic crises that are well recorded in the numerous a