Zobrazeno 1 - 4
of 4
pro vyhledávání: '"Tatiana B. Kolotilina"'
Publikováno v:
Minerals, Vol 14, Iss 3, p 290 (2024)
The Lysan alkaline–ultramafic complex is located in the Sisim shear zone at the contact of the two largest tectonic structures of the accretion–collisional belt in the southwestern frame of the Siberian craton. Intrusions of the complex consist o
Externí odkaz:
https://doaj.org/article/63b20a600a0649079d75d09465ccbbe7
Publikováno v:
Minerals, Vol 10, Iss 7, p 608 (2020)
Composition variations of Cr-spinel in high-Mg rocks of the Primorsky Ridge (Western Baikal region, Russia) are reported here. A specific feature of Cr-spinels in ultramafic rocks of the Primorsky Ridge is their noticeably high Ti content (up to 6.5
Externí odkaz:
https://doaj.org/article/f9fb8c33e45f47abbf8d231cc5c225dd
Publikováno v:
Minerals, Vol 9, Iss 8, p 479 (2019)
Re sulfides were discovered in Cu−Ni−platinum-group elements (PGE) ores of the Zhelos and Tokty-Oi intrusions. These intrusions can be considered as products of the mantle superplume responsible for Rodinia’s break-up. The mineral compositions
Externí odkaz:
https://doaj.org/article/b43da99fc37b4200b2eaeefb52b1587e
Publikováno v:
Minerals, Vol 9, Iss 8, p 479 (2019)
Minerals
Volume 9
Issue 8
Minerals
Volume 9
Issue 8
Re sulfides were discovered in Cu&ndash
Ni&ndash
platinum-group elements (PGE) ores of the Zhelos and Tokty-Oi intrusions. These intrusions can be considered as products of the mantle superplume responsible for Rodinia&rsquo
s break-up
Ni&ndash
platinum-group elements (PGE) ores of the Zhelos and Tokty-Oi intrusions. These intrusions can be considered as products of the mantle superplume responsible for Rodinia&rsquo
s break-up