Standard

The geochemical model for forming of Li-F granites of the Orlovsky deposit (Eastern Transbaikal). / Syritso, L. F.; Tabuns, E. V.; Badanina, E. V.

In: Vestnik - Sankt-Petersburgskogo Universiteta, Seriya Geologiya i Geografiya, Vol. 8, No. 2, 01.12.1999, p. 65-69.

Research output: Contribution to journal › Article › peer-review

Harvard

Syritso, LF, Tabuns, EV & Badanina, EV 1999, 'The geochemical model for forming of Li-F granites of the Orlovsky deposit (Eastern Transbaikal)', Vestnik - Sankt-Petersburgskogo Universiteta, Seriya Geologiya i Geografiya, vol. 8, no. 2, pp. 65-69.

APA

Syritso, L. F., Tabuns, E. V., & Badanina, E. V. (1999). The geochemical model for forming of Li-F granites of the Orlovsky deposit (Eastern Transbaikal). Vestnik - Sankt-Petersburgskogo Universiteta, Seriya Geologiya i Geografiya, 8(2), 65-69.

Vancouver

Syritso LF, Tabuns EV, Badanina EV. The geochemical model for forming of Li-F granites of the Orlovsky deposit (Eastern Transbaikal). Vestnik - Sankt-Petersburgskogo Universiteta, Seriya Geologiya i Geografiya. 1999 Dec 1;8(2):65-69.

Author

Syritso, L. F. ; Tabuns, E. V. ; Badanina, E. V. / The geochemical model for forming of Li-F granites of the Orlovsky deposit (Eastern Transbaikal). In: Vestnik - Sankt-Petersburgskogo Universiteta, Seriya Geologiya i Geografiya. 1999 ; Vol. 8, No. 2. pp. 65-69.

BibTeX

@article{b2bfe9c0540d40ebabc502a73cc28df2,
title = "The geochemical model for forming of Li-F granites of the Orlovsky deposit (Eastern Transbaikal)",
abstract = "The quantitative geochemical model for origin of Li-F granites of the Orlovsky deposit (Eastern Tansbaikal) has been developed. Mineral-forming media composition (rock-forming elements, Li, Rb, Cs, Ta, Nb, W, Sr, Zr, Ba, F) for the different evolution stages of Orlovka granite massif was estimated on the basis of the mass balance calculation taking into account rock composition, spatial and volumeric relationships. An effective integral partition coefficients of Fe, Mn, K, Na, Li, Rb, Cs, Ta, Nb, W, Sr, Zr, Ba, F and partition coefficients between magma and potassic feldspar, mica, quartz and Zr were determined. These data conform with the results, obtained by the conventional method of investigation.",
author = "Syritso, {L. F.} and Tabuns, {E. V.} and Badanina, {E. V.}",
year = "1999",
month = dec,
day = "1",
language = "English",
volume = "8",
pages = "65--69",
journal = "Вестник Санкт-Петербургского университета. Науки о Земле",
issn = "1812-9323",
publisher = "Издательство Санкт-Петербургского университета",
number = "2",

}

RIS

TY - JOUR

T1 - The geochemical model for forming of Li-F granites of the Orlovsky deposit (Eastern Transbaikal)

AU - Syritso, L. F.

AU - Tabuns, E. V.

AU - Badanina, E. V.

PY - 1999/12/1

Y1 - 1999/12/1

N2 - The quantitative geochemical model for origin of Li-F granites of the Orlovsky deposit (Eastern Tansbaikal) has been developed. Mineral-forming media composition (rock-forming elements, Li, Rb, Cs, Ta, Nb, W, Sr, Zr, Ba, F) for the different evolution stages of Orlovka granite massif was estimated on the basis of the mass balance calculation taking into account rock composition, spatial and volumeric relationships. An effective integral partition coefficients of Fe, Mn, K, Na, Li, Rb, Cs, Ta, Nb, W, Sr, Zr, Ba, F and partition coefficients between magma and potassic feldspar, mica, quartz and Zr were determined. These data conform with the results, obtained by the conventional method of investigation.

AB - The quantitative geochemical model for origin of Li-F granites of the Orlovsky deposit (Eastern Tansbaikal) has been developed. Mineral-forming media composition (rock-forming elements, Li, Rb, Cs, Ta, Nb, W, Sr, Zr, Ba, F) for the different evolution stages of Orlovka granite massif was estimated on the basis of the mass balance calculation taking into account rock composition, spatial and volumeric relationships. An effective integral partition coefficients of Fe, Mn, K, Na, Li, Rb, Cs, Ta, Nb, W, Sr, Zr, Ba, F and partition coefficients between magma and potassic feldspar, mica, quartz and Zr were determined. These data conform with the results, obtained by the conventional method of investigation.

UR - http://www.scopus.com/inward/record.url?scp=0033504925&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:0033504925

VL - 8

SP - 65

EP - 69

JO - Вестник Санкт-Петербургского университета. Науки о Земле

JF - Вестник Санкт-Петербургского университета. Науки о Земле

SN - 1812-9323

IS - 2

ER -

ID: 50679387