Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
Fluid inclusions in zoisite of the Merelani hills deposit, Tanzaniya. / Kazantseva, M. I.; Ponomareva, N. I.; Bocharov, V. N.
в: Zapiski Rossiiskogo Mineralogicheskogo Obshchestva, Том 147, № 3, 01.01.2018, стр. 69-81.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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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