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Fluid inclusions in zoisite of the Merelani hills deposit, Tanzaniya. / Kazantseva, M. I.; Ponomareva, N. I.; Bocharov, V. N.

In: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Vol. 147, No. 3, 01.01.2018, p. 69-81.

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

Harvard

Kazantseva, MI, Ponomareva, NI & Bocharov, VN 2018, 'Fluid inclusions in zoisite of the Merelani hills deposit, Tanzaniya', Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, vol. 147, no. 3, pp. 69-81. https://doi.org/10.30695/zrmo/2018.1473.05

APA

Kazantseva, M. I., Ponomareva, N. I., & Bocharov, V. N. (2018). Fluid inclusions in zoisite of the Merelani hills deposit, Tanzaniya. Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, 147(3), 69-81. https://doi.org/10.30695/zrmo/2018.1473.05

Vancouver

Kazantseva MI, Ponomareva NI, Bocharov VN. Fluid inclusions in zoisite of the Merelani hills deposit, Tanzaniya. Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2018 Jan 1;147(3):69-81. https://doi.org/10.30695/zrmo/2018.1473.05

Author

Kazantseva, M. I. ; Ponomareva, N. I. ; Bocharov, V. N. / Fluid inclusions in zoisite of the Merelani hills deposit, Tanzaniya. In: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva. 2018 ; Vol. 147, No. 3. pp. 69-81.

BibTeX

@article{c74a75986a2b43a199b75f4b036d21dc,
title = "Fluid inclusions in zoisite of the Merelani hills deposit, Tanzaniya",
abstract = " The study was focused upon fluid inclusions in zoisite from the Merelani Hills deposit (Northern Tanzania) - they are characterized by the unique composition. The Raman spectroscopy has detected there mostly the system H 2 S) (N 2 )) (CH 4 ), together with remarked presence of liquid H 2 O and the ion HS - . Solid phases in inclusions are identified as graphite, calcite, quartz, dickite, micas, and the native sulfur (S 8 ). The average temperature of partial homogenization corresponds for gas-liquid inclusions, according to authors, is equal to 60-70 °C, complete homogenization and dissolution of solid phases occurs at temperature about 400 °C (Malisa et al., 1986). Physical-chemical parameters of the zoisite formation were estimated with techniques of chemical thermodynamic calculation: Eh 7 -0.2; pH 7 6.4. ",
keywords = "Fluid inclusions, Merelani Hills deposit, Mineralization conditions, Raman spectroscopy, Zoisite",
author = "Kazantseva, {M. I.} and Ponomareva, {N. I.} and Bocharov, {V. N.}",
year = "2018",
month = jan,
day = "1",
doi = "10.30695/zrmo/2018.1473.05",
language = "English",
volume = "147",
pages = "69--81",
journal = "ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА",
issn = "0869-6055",
publisher = "Издательство {"}Наука{"}",
number = "3",

}

RIS

TY - JOUR

T1 - Fluid inclusions in zoisite of the Merelani hills deposit, Tanzaniya

AU - Kazantseva, M. I.

AU - Ponomareva, N. I.

AU - Bocharov, V. N.

PY - 2018/1/1

Y1 - 2018/1/1

N2 - The study was focused upon fluid inclusions in zoisite from the Merelani Hills deposit (Northern Tanzania) - they are characterized by the unique composition. The Raman spectroscopy has detected there mostly the system H 2 S) (N 2 )) (CH 4 ), together with remarked presence of liquid H 2 O and the ion HS - . Solid phases in inclusions are identified as graphite, calcite, quartz, dickite, micas, and the native sulfur (S 8 ). The average temperature of partial homogenization corresponds for gas-liquid inclusions, according to authors, is equal to 60-70 °C, complete homogenization and dissolution of solid phases occurs at temperature about 400 °C (Malisa et al., 1986). Physical-chemical parameters of the zoisite formation were estimated with techniques of chemical thermodynamic calculation: Eh 7 -0.2; pH 7 6.4.

AB - The study was focused upon fluid inclusions in zoisite from the Merelani Hills deposit (Northern Tanzania) - they are characterized by the unique composition. The Raman spectroscopy has detected there mostly the system H 2 S) (N 2 )) (CH 4 ), together with remarked presence of liquid H 2 O and the ion HS - . Solid phases in inclusions are identified as graphite, calcite, quartz, dickite, micas, and the native sulfur (S 8 ). The average temperature of partial homogenization corresponds for gas-liquid inclusions, according to authors, is equal to 60-70 °C, complete homogenization and dissolution of solid phases occurs at temperature about 400 °C (Malisa et al., 1986). Physical-chemical parameters of the zoisite formation were estimated with techniques of chemical thermodynamic calculation: Eh 7 -0.2; pH 7 6.4.

KW - Fluid inclusions

KW - Merelani Hills deposit

KW - Mineralization conditions

KW - Raman spectroscopy

KW - Zoisite

UR - http://www.scopus.com/inward/record.url?scp=85063754054&partnerID=8YFLogxK

U2 - 10.30695/zrmo/2018.1473.05

DO - 10.30695/zrmo/2018.1473.05

M3 - Article

AN - SCOPUS:85063754054

VL - 147

SP - 69

EP - 81

JO - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

JF - ЗАПИСКИ РОССИЙСКОГО МИНЕРАЛОГИЧЕСКОГО ОБЩЕСТВА

SN - 0869-6055

IS - 3

ER -

ID: 49681858