Standard

Specific features of scapolite-bearing assemblage formation : Oxygen isotope evidence. / Ustinov, V. I.; Zolotarev, A. A.; Ul'Yanov, A. A.

в: Geokhimiya, Том 35, № 5, 1997, стр. 533-534.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Ustinov, VI, Zolotarev, AA & Ul'Yanov, AA 1997, 'Specific features of scapolite-bearing assemblage formation: Oxygen isotope evidence', Geokhimiya, Том. 35, № 5, стр. 533-534.

APA

Ustinov, V. I., Zolotarev, A. A., & Ul'Yanov, A. A. (1997). Specific features of scapolite-bearing assemblage formation: Oxygen isotope evidence. Geokhimiya, 35(5), 533-534.

Vancouver

Ustinov VI, Zolotarev AA, Ul'Yanov AA. Specific features of scapolite-bearing assemblage formation: Oxygen isotope evidence. Geokhimiya. 1997;35(5):533-534.

Author

Ustinov, V. I. ; Zolotarev, A. A. ; Ul'Yanov, A. A. / Specific features of scapolite-bearing assemblage formation : Oxygen isotope evidence. в: Geokhimiya. 1997 ; Том 35, № 5. стр. 533-534.

BibTeX

@article{b5a0eaddbbc54c4c9f19ddf840ce6e74,
title = "Specific features of scapolite-bearing assemblage formation: Oxygen isotope evidence",
abstract = "In addition to the elaboration of monomineral isotopic geothermometers, the combination of intra- and inframineral studies of oxygen isotope distribution is one important application of the intrastructural isotopic method in genetic mineralogy and geochemistry, which allows us to specify the formation conditions of mineral assemblages and to clarify the mineral-formation mechanisms.",
author = "Ustinov, {V. I.} and Zolotarev, {A. A.} and Ul'Yanov, {A. A.}",
year = "1997",
language = "English",
volume = "35",
pages = "533--534",
journal = "ГЕОХИМИЯ",
issn = "0016-7525",
publisher = "Издательство {"}Наука{"}",
number = "5",

}

RIS

TY - JOUR

T1 - Specific features of scapolite-bearing assemblage formation

T2 - Oxygen isotope evidence

AU - Ustinov, V. I.

AU - Zolotarev, A. A.

AU - Ul'Yanov, A. A.

PY - 1997

Y1 - 1997

N2 - In addition to the elaboration of monomineral isotopic geothermometers, the combination of intra- and inframineral studies of oxygen isotope distribution is one important application of the intrastructural isotopic method in genetic mineralogy and geochemistry, which allows us to specify the formation conditions of mineral assemblages and to clarify the mineral-formation mechanisms.

AB - In addition to the elaboration of monomineral isotopic geothermometers, the combination of intra- and inframineral studies of oxygen isotope distribution is one important application of the intrastructural isotopic method in genetic mineralogy and geochemistry, which allows us to specify the formation conditions of mineral assemblages and to clarify the mineral-formation mechanisms.

UR - http://www.scopus.com/inward/record.url?scp=33746257666&partnerID=8YFLogxK

M3 - Article

AN - SCOPUS:33746257666

VL - 35

SP - 533

EP - 534

JO - ГЕОХИМИЯ

JF - ГЕОХИМИЯ

SN - 0016-7525

IS - 5

ER -

ID: 9332717