Zobrazeno 1 - 8
of 8
pro vyhledávání: '"Anna Firstova"'
Autor:
Anna Firstova, Georgy Cherkashov, Tamara Stepanova, Anna Sukhanova, Irina Poroshina, Victor Bel’tenev
Publikováno v:
Minerals, Vol 12, Iss 12, p 1593 (2022)
The internal structure of Seafloor Massive Sulfides (SMS) deposits is one of the most important and complex issues facing the study of modern hydrothermal ore systems. The Semenov-5 hydrothermal field is a unique area where mass wasting on the slope
Externí odkaz:
https://doaj.org/article/d3ca47701cc3463185de89cb50f530e0
Autor:
Valeriy V. Maslennikov, Georgy Cherkashov, Dmitry A. Artemyev, Anna Firstova, Ross R. Large, Aleksandr Tseluyko, Vasiliy Kotlyarov
Publikováno v:
Minerals, Vol 10, Iss 7, p 622 (2020)
The massive sulfide ores of the Pobeda hydrothermal fields are grouped into five main mineral microfacies: (1) isocubanite-pyrite, (2) pyrite-wurtzite-isocubanite, (3) pyrite with minor isocubanite and wurtzite-sphalerite microinclusions, (4) pyrite-
Externí odkaz:
https://doaj.org/article/e344d584a5754dac8a6a827997c582b4
Publikováno v:
Minerals, Vol 9, Iss 5, p 294 (2019)
The Semyenov-2 hydrothermal field located at 13°31′N of the Mid-Atlantic Ridge (MAR) is associated with an oceanic core complex (OCC) and hosted by peridotites and basalts with minor amounts of gabbro and plagiogranites. Seafloor massive sulphides
Externí odkaz:
https://doaj.org/article/d58f1d74062642e9ba0ec514c43bd239
Publikováno v:
Minerals, Vol 6, Iss 1, p 19 (2016)
This paper presents mineralogical and geochemical data on seafloor massive sulfides (SMS) from the Ashadze-1 hydrothermal field at the Mid-Atlantic Ridge (MAR). The Ashadze-1 deposit is associated with the uplifted lower crust and upper mantle (ocean
Externí odkaz:
https://doaj.org/article/f5d6805a92b94bdeb63aa2747d5df2ae
Autor:
Vasiliy A. Kotlyarov, Valeriy V. Maslennikov, A. S. Tseluyko, Dmitry A. Artemyev, Ross R. Large, Anna Firstova, Georgy Cherkashov
Publikováno v:
Minerals, Vol 10, Iss 622, p 622 (2020)
Minerals
Volume 10
Issue 7
Minerals
Volume 10
Issue 7
The massive sulfide ores of the Pobeda hydrothermal fields are grouped into five main mineral microfacies: (1) isocubanite-pyrite, (2) pyrite-wurtzite-isocubanite, (3) pyrite with minor isocubanite and wurtzite-sphalerite microinclusions, (4) pyrite-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2384c318399384da421e9df349795b75
https://www.mdpi.com/2075-163X/10/7/622
https://www.mdpi.com/2075-163X/10/7/622
Autor:
Georgy Cherkashov, Anna Firstova, Artem Bich, V. E. Bel’tenev, Katherine Kuksa, Vladislav Kuznetsov
Publikováno v:
Marine Geology. 438:106517
Metalliferous sediments associated with oceanic hydrothermal systems contain various amounts of metals of a dual origin: from suspended particulate matter of an overlying plume and from weathered massive sulfide edifices. This study investigates the
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::21d2e2b1727078b4e4fc57870df843f2
https://doi.org/10.1016/j.margeo.2021.106517
https://doi.org/10.1016/j.margeo.2021.106517
Publikováno v:
Minerals
Volume 9
Issue 5
Minerals, Vol 9, Iss 5, p 294 (2019)
Volume 9
Issue 5
Minerals, Vol 9, Iss 5, p 294 (2019)
The Semyenov-2 hydrothermal field located at 13°
31&prime
N of the Mid-Atlantic Ridge (MAR) is associated with an oceanic core complex (OCC) and hosted by peridotites and basalts with minor amounts of gabbro and plagiogranites. Seafloor
31&prime
N of the Mid-Atlantic Ridge (MAR) is associated with an oceanic core complex (OCC) and hosted by peridotites and basalts with minor amounts of gabbro and plagiogranites. Seafloor
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::cce0d83bcdd6d9b01a89fd65b781bb73
https://doi.org/10.3390/min9050294
https://doi.org/10.3390/min9050294
Publikováno v:
Minerals; Volume 6; Issue 1; Pages: 19
Minerals, Vol 6, Iss 1, p 19 (2016)
Minerals, Vol 6, Iss 1, p 19 (2016)
This paper presents mineralogical and geochemical data on seafloor massive sulfides (SMS) from the Ashadze-1 hydrothermal field at the Mid-Atlantic Ridge (MAR). The Ashadze-1 deposit is associated with the uplifted lower crust and upper mantle (ocean
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::7b20e1089e2e03602adfe80c6bdeb5af
https://doi.org/10.3390/min6010019
https://doi.org/10.3390/min6010019