Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Svetlana N. Shanina"'
Publikováno v:
Minerals, Vol 13, Iss 6, p 781 (2023)
Lode gold deposits are widespread in orogenic belts of various ages and are a valuable gold source, but their genesis remains debatable. The close relationship between native gold and quartz was considered a reason to search for acid-magmatic sources
Externí odkaz:
https://doaj.org/article/16b3013a78324ce690db4b3fb7012814
Autor:
Valerii V. Murzin, Svetlana N. Shanina
Publikováno v:
Литосфера, Vol 17, Iss 6, Pp 110-117 (2017)
In the paper, there are adduced the data of a thermobarogeochemistry investigation of fluid inclusions in apatite of magnetite-chlorite-carbonates rocks from ultrabasite Karabash massife. The rocks are carrying copper-bearing aurum (1.3-2.6 wt % Cu)
Externí odkaz:
https://doaj.org/article/9614ce2a475246e2b5d3cfa1dc79e014
Publikováno v:
Journal of Earth Science. 31:514-522
The P-T conditions of auriferous and barren quartz veins from Kopylovsky, Kavkaz and Krasnoye gold deposits in Proterozoic black shales of Bodaybo ore region are presented the first time in this study. Fluid inclusions trapped in auriferous quartz ar
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1c40956c1aa1ed6f527ab8a716a6f126
https://doi.org/10.1007/s12583-019-1024-5
https://doi.org/10.1007/s12583-019-1024-5
Publikováno v:
Zapiski RMO (Proceedings of the Russian Mineralogical Society). 148:95-109
The study of the amino acid composition of gallstones of the Komi Republic residents has shown the significant differences in cholesterol and pigment specimens. It has been revealed that during formation of the carbonate or phosphate component in gal
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5f6c7aa0c7dcdea33f6b8a939734ba11
https://doi.org/10.30695/zrmo/2019.1484.07
https://doi.org/10.30695/zrmo/2019.1484.07
Publikováno v:
Springer Proceedings in Earth and Environmental Sciences ISBN: 9783030494674
The chemical and amino acid composition of gallstones of cholesterol, mixed (cholesterol + mineral component (calcium carbonate, calcium phosphate)), and pigment types was studied. The Mann-Whitney test revealed statistically significant differences
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::027ed8a3babe9a413179efadd2821b1d
https://doi.org/10.1007/978-3-030-49468-1_18
https://doi.org/10.1007/978-3-030-49468-1_18
Autor:
Svetlana N. Shanina, Valerii V. Murzin
Publikováno v:
Литосфера, Vol 17, Iss 6, Pp 110-117 (2017)
In the paper, there are adduced the data of a thermobarogeochemistry investigation of fluid inclusions in apatite of magnetite-chlorite-carbonates rocks from ultrabasite Karabash massife. The rocks are carrying copper-bearing aurum (1.3-2.6 wt % Cu)
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::ac27ddfa0d239d2f3fd44077ddaec201
https://www.lithosphere.ru/jour/article/view/128
https://www.lithosphere.ru/jour/article/view/128
Autor:
Аnatolіy R. Galamay, Oleg O. Ignatovich, Fanwei Meng, Pei Ni, Svetlana N. Shanina, Krzysztof Bukowski
Publikováno v:
Geological Quarterly.
This study describes a new determination of the S and O isotope composition of Lower Permian (Kungurian) anhydrites from the Upper Pechora Basin, Cis-Ural region, Russia. δ 34 S values in sulphate facies vary from +13.7 to +15.1‰; and δ 18 O valu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eb01f8365ab5e0c2e4ce3ddd54b4ca8d
https://doi.org/10.7306/gq.1309
https://doi.org/10.7306/gq.1309
Autor:
Svetlana N. Shanina
Publikováno v:
SPIE Proceedings.
It was established that the same type of organic matter was accumulated in ancient salts independently of their ages and mineralogical compositions. The origin of hydrocarbons of salt bitumoids was aquagennic organic matter, which accumulated in rest
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1b8d356dd7243a5ab612178c13ead381
https://doi.org/10.1117/12.486692
https://doi.org/10.1117/12.486692