Zobrazeno 1 - 10
of 49
pro vyhledávání: '"Andrei V. Girnis"'
Publikováno v:
Geochemistry International. 58:271-290
The mean concentrations of volatiles, major, and trace elements are estimated in the magmatic melts of Kamchatka based on an our database that includes analyses of melt inclusions and quenched glasses of rocks for 75 elements (the database comprised
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::a5d357c1f6d619d6e4b5fe87a99369b5
https://doi.org/10.1134/s001670292003009x
https://doi.org/10.1134/s001670292003009x
Publikováno v:
Геохимия. 64:395-408
As a continuation of our previous study, we estimated the mean contents of volatile, major, and trace components in silicic (>66 wt % SiO2) magmatic melts from main terrestrial geodynamic settings on the basis of our database, which includes (as of m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b0e297809fc34cc657b67e6b9aec9ca
https://doi.org/10.31857/s0016-7525644395-408
https://doi.org/10.31857/s0016-7525644395-408
Publikováno v:
Geochemistry International. 57:407-423
Continuing our earlier publication, this paper presents estimates (based on our database, which included more than 1 500 000 analyses of melt inclusions and chilled glasses of rocks for 75 elements, as of 2017) of the mean concentrations of volatile,
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ecc75474375b700ef710236c47704aa2
https://doi.org/10.1134/s0016702919040086
https://doi.org/10.1134/s0016702919040086
Publikováno v:
Chemical Geology. 505:12-22
Sulfur solubility in Ca–Mg–Fe silicate–carbonate melt was experimentally determined at 5–10.5 GPa and 1400–1600 °C. Melt was produced by reaction between natural carbonates (calcite and magnesite) and San Carlos olivine (XFo ~ 0.9), which
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c28ddd3c93e5d2433ae1f6b53e95c7f0
https://doi.org/10.1016/j.chemgeo.2018.12.008
https://doi.org/10.1016/j.chemgeo.2018.12.008
Publikováno v:
Lithos. :302-313
Diamond nucleation and growth were investigated experimentally at 7.5 and 10.5 GPa and temperatures up to 1500 °C. Samples consisted of two layers: i) H2O- and CO2-bearing model sediment and ii) graphite-bearing garnet harzburgite comprising natural
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0ba53869bcbb1e8d76107dd0935a9532
https://doi.org/10.1016/j.lithos.2018.04.010
https://doi.org/10.1016/j.lithos.2018.04.010
Publikováno v:
Geochemistry International. 55:629-653
Mean concentrations of major components, trace elements, and volatile components in magmatic melts from Earth’s major geodynamic environments are estimated using our database (which comprises more than 1200000 analyses for 75 chemical elements—st
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::733969d5e4e1203e0372298e42a49c22
https://doi.org/10.1134/s0016702917070060
https://doi.org/10.1134/s0016702917070060
Publikováno v:
Contributions to Mineralogy and Petrology. 174
Ferropericlase is a common lower mantle phase that can occur as inclusions in “superdeep” diamonds. However, it has been proposed that some of these inclusions could be formed in the upper mantle (Brey et al. 2004). To explore this hypothesis, tw
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::28e3f323a18df09ce6e26637d67ca488
https://doi.org/10.1007/s00410-019-1582-6
https://doi.org/10.1007/s00410-019-1582-6
Publikováno v:
International Kimberlite Conference Extended Abstracts: 2008.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::87753b5b434be6db57731d167dea7abe
https://doi.org/10.29173/ikc3253
https://doi.org/10.29173/ikc3253
Publikováno v:
International Kimberlite Conference Extended Abstracts: 1995.
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c8ef4062402686f5b37065dd5d3d12f3
https://doi.org/10.29173/ikc1788
https://doi.org/10.29173/ikc1788
Publikováno v:
Geochemistry International. 54:543-558
Our database of published contents of volatile, major, and trace elements in melt inclusions in minerals and quenched glasses of volcanic rocks was used to calculate the mean compositions of alkaline and subalkaline melts of ocean islands. The data a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::51c90ba88628e7176d5e3d779dbfe272
https://doi.org/10.1134/s0016702916040066
https://doi.org/10.1134/s0016702916040066