Zobrazeno 1 - 5
of 5
pro vyhledávání: '"V. S. Kamenetsky"'
Publikováno v:
Геодинамика и тектонофизика, Vol 12, Iss 4, Pp 883-890 (2021)
The paper considers the Pd/Pt ratio in the ores of the Norilsk-1 and Talnakh deposits associated with the Permian-Triassic intrusions of the Norilsk type in comparison with that in the lavas of the same age in the Norilsk region. The Pd/Pt mean ratio
Externí odkaz:
https://doaj.org/article/1becac908ac84cc588e8678eec769e50
Publikováno v:
Geochemistry, Geophysics, Geosystems, Vol 21, Iss 2, Pp n/a-n/a (2020)
Abstract Intense emission of volcanic aerosol accompanied the 2012–2013 basaltic effusive eruption of Tolbachik volcano, Kamchatka. The aerosols sampled contain sulfuric acid droplets, glassy particles, and 70 mineral phases. All aerosol particles
Externí odkaz:
https://doaj.org/article/bd456718fc3d4a6eb9a1e082235b5034
Autor:
E. P. Shevko, S. B. Bortnikova, N. A. Abrosimova, V. S. Kamenetsky, S. P. Bortnikova, G. L. Panin, M. Zelenski
Publikováno v:
Geofluids, Vol 2018 (2018)
Native sulfur deposits on fumarolic fields at Ebeko volcano (Northern Kuriles, Russia) are enriched in chalcophile elements (As-Sb-Se-Te-Hg-Cu) and contain rare heavy metal sulfides (Ag2S, HgS, and CuS), native metal alloys (Au2Pd), and some other lo
Externí odkaz:
https://doaj.org/article/38fae974a12149a8818f6ab59ff3572d
Publikováno v:
WATER-ROCK INTERACTION: GEOLOGICAL EVOLUTION
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::1a75c2e0bc401a75136e0982f6d2bfba
https://doi.org/10.31554/978-5-7925-0584-1-2020-351-354
https://doi.org/10.31554/978-5-7925-0584-1-2020-351-354
Autor:
A. V. Sobolev, Ann-Karolin Hofmann, Stephan V. Sobolev, I. K. Nikogosian, D. V. Kuzmin, A. A. Gurenko, V. S. Kamenetsky, N. A. Krivolutskaya
Publikováno v:
EOS, Transactions, American Geophysical Union, Suppl. ; Vol. 85, 47
AGU 2004 Fall Meeting (San Francisco 2004)#
AGU 2004 Fall Meeting (San Francisco 2004)#
The role of recycled material in mantle plumes is difficult to quantify on the basis of incompatible trace elements and isotopes because of the great variability of subducted material. Another approach is to use major elements and compatible trace el
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::751cbd7ef70204c065119d70e01fbcb9
https://gfzpublic.gfz-potsdam.de/pubman/item/item_232678
https://gfzpublic.gfz-potsdam.de/pubman/item/item_232678