Zobrazeno 1 - 10
of 13
pro vyhledávání: '"T. N. Shuriga"'
Publikováno v:
Geology of Ore Deposits. 53:390-400
The Snezhnoe phenakite-beryl deposit is one of the highest-grade deposits in the Altai-Sayan beryllium province. This deposit is spatially associated with the alkali granite of the Ognit Complex and localized in the apical part of the granitic pluton
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6e85b19b094b5cbe5568481fc87e0ac6
https://doi.org/10.1134/s1075701511040064
https://doi.org/10.1134/s1075701511040064
Autor:
V. V. Yarmolyuk, T. N. Shuriga, E. B. Sal’nikova, A. V. Travin, A. M. Kozlovskiy, A. V. Nikiforov, V. I. Lebedev, D. A. Lykhin, Yu. V. Plotkina, I. V. Anisimova, S. Z. Yakovleva, A. B. Kotov
Publikováno v:
Doklady Earth Sciences. 430:95-100
95 Raremetal magmatism covering the age range of more than 1 billion years, from the Late Riphean to the Triassic, is widely abundant within the southern margin of the Siberian Platform and its folded sur� rounding. Late Riphean massifs of alkali-u
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::967ecc3399ee7c279def5861f9cf4076
https://doi.org/10.1134/s1028334x10010216
https://doi.org/10.1134/s1028334x10010216
Autor:
L. T. Rakov, T. N. Shuriga
Publikováno v:
Geochemistry International. 47:1021-1035
A reliable criterion of quartz genesis is proved to be ratios of the concentrations of structural defects in this mineral, which are a function of its structural dynamic state. Within the scope of the theory of sparring defects, theoretical dependenc
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8fbfd3096984ac80fc286ccd2026e062
https://doi.org/10.1134/s0016702909100061
https://doi.org/10.1134/s0016702909100061
Publikováno v:
Geochemistry International. 47:526-529
K ( Al )[ Al 2 Si 2 O 10 ]( OH ) 2 isomorphous series. The micas of zinnwaldite composition contain 3–4% Li 2 O, and protolithionites have higher Fe and lower Li 2 O (1–3%) contents. These minerals typically occur in rare-metal granites, granite
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f5bba4856f92887932b6cd5190dbbe6c
https://doi.org/10.1134/s0016702909050097
https://doi.org/10.1134/s0016702909050097
Publikováno v:
Geochemistry International. 47:174-185
The paper proposes pioneering data on the polarized optical absorption spectra of Li-Fe micas: intermediate members of the siderophyllite-zinnwaldite-polylithionite and annite-protolithionite-zinnwaldite-trilithionite series with variable Fe and Li p
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::81c35073876d171b3deef18ca7af5c89
https://doi.org/10.1134/s0016702909020050
https://doi.org/10.1134/s0016702909020050
Publikováno v:
Russian Journal of Physical Chemistry A. 83:346-349
A thermochemical study of lithium siderophyllite (K0.75Na0.06Rb0.01Ca0.11)(Li0.11Fe1.252+Mn0.02Mg0.66Al0.35Fe0.233+Ti0.18)[Si2.53Al1.47O10](OH)1.63F0.37 (I) and siderophyllite (Al-Fe biotite) (K0.89Na0.04)(Fe1.692+Mn0.03Mg0.20Al0.59Fe0.143+Ti0.06)[Si
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6911e891e92209a6b27a8e4d04142b39
https://doi.org/10.1134/s0036024409030042
https://doi.org/10.1134/s0036024409030042
Publikováno v:
Geochemistry International. 47:105-108
Biotites are widespread trioctahedral Mg‐Fe micas that are intermediate members of the phlogopite‐annite join. Pure annite K [ Si 3 AlO 10 ]( OH ) 2 is known only as a synthetic compound; natural annites typically contain no more than 2.0‐2.5 f
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::e1a9a6c159699ae2baa4710bc0fa15b7
https://doi.org/10.1134/s001670290901008x
https://doi.org/10.1134/s001670290901008x
Publikováno v:
Russian Journal of Physical Chemistry A. 82:942-945
A thermochemical study of natural lithium micas, iron-containing polylithionite and lepidolite, was performed on a high-temperature heat-flux Calvet microcalorimeter (Setaram, France). Melt solution calorimetry was used to measure the enthalpies of m
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ceff522059c3d13aafb9a1479c9f3a6d
https://doi.org/10.1134/s0036024408060137
https://doi.org/10.1134/s0036024408060137
Publikováno v:
Geochemistry International. 45:926-930
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::0c9012f08712183a7a8a4b694190d4d9
https://doi.org/10.1134/s0016702907090066
https://doi.org/10.1134/s0016702907090066
Publikováno v:
Geochemistry International. 45:501-505
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d9454681d053f8202b2a9dc63aa6e8e7
https://doi.org/10.1134/s0016702907050072
https://doi.org/10.1134/s0016702907050072