Standard

Chemical composition and varieties of sulfosalts from gold mineralization in the Gaching ore occurrence (Maletoyvayam ore field). / Shapovalova, M.; Tolstykh, N.; Bobrova, O.

In: IOP Conference Series: Earth and Environmental Science, Vol. 319, No. 1, 012019, 19.09.2019.

Research output: Contribution to journalConference articlepeer-review

Harvard

Shapovalova, M, Tolstykh, N & Bobrova, O 2019, 'Chemical composition and varieties of sulfosalts from gold mineralization in the Gaching ore occurrence (Maletoyvayam ore field)', IOP Conference Series: Earth and Environmental Science, vol. 319, no. 1, 012019. https://doi.org/10.1088/1755-1315/319/1/012019

APA

Shapovalova, M., Tolstykh, N., & Bobrova, O. (2019). Chemical composition and varieties of sulfosalts from gold mineralization in the Gaching ore occurrence (Maletoyvayam ore field). IOP Conference Series: Earth and Environmental Science, 319(1), [012019]. https://doi.org/10.1088/1755-1315/319/1/012019

Vancouver

Shapovalova M, Tolstykh N, Bobrova O. Chemical composition and varieties of sulfosalts from gold mineralization in the Gaching ore occurrence (Maletoyvayam ore field). IOP Conference Series: Earth and Environmental Science. 2019 Sept 19;319(1):012019. doi: 10.1088/1755-1315/319/1/012019

Author

Shapovalova, M. ; Tolstykh, N. ; Bobrova, O. / Chemical composition and varieties of sulfosalts from gold mineralization in the Gaching ore occurrence (Maletoyvayam ore field). In: IOP Conference Series: Earth and Environmental Science. 2019 ; Vol. 319, No. 1.

BibTeX

@article{7b3a9d045a18482dbc571de42227db4d,
title = "Chemical composition and varieties of sulfosalts from gold mineralization in the Gaching ore occurrence (Maletoyvayam ore field)",
abstract = "The Gaching ore occurrence within the Maletoyvayam ore field is located in the southwestern part of Kamchatka volcanic belt. The ore occurrence belongs to high-sulfidation epithermal type. The sulfosalts of the fahlore-group (tennantite, tetrahedrites and goldfieldite) and enargite-groups (enargite, luzonite, famatinite) found in the gold mineralization of the Gaching ore occurrence. The presence of Cu-rich and Se-bearing fahlores as well as enargite-group sulfosalts in ores indicate a high oxygen volatility at temperature less than 250° during their formation.",
keywords = "GOLDFIELDITE, CHEMISTRY, MINERALS, RHODOPE",
author = "M. Shapovalova and N. Tolstykh and O. Bobrova",
year = "2019",
month = sep,
day = "19",
doi = "10.1088/1755-1315/319/1/012019",
language = "English",
volume = "319",
journal = "IOP Conference Series: Earth and Environmental Science",
issn = "1755-1307",
publisher = "IOP Publishing Ltd.",
number = "1",
note = "10th All Russian Petrographic Conference with International Participationon Petrology of Magnetic and Metamorphic Complexes ; Conference date: 27-11-2018 Through 28-11-2018",

}

RIS

TY - JOUR

T1 - Chemical composition and varieties of sulfosalts from gold mineralization in the Gaching ore occurrence (Maletoyvayam ore field)

AU - Shapovalova, M.

AU - Tolstykh, N.

AU - Bobrova, O.

PY - 2019/9/19

Y1 - 2019/9/19

N2 - The Gaching ore occurrence within the Maletoyvayam ore field is located in the southwestern part of Kamchatka volcanic belt. The ore occurrence belongs to high-sulfidation epithermal type. The sulfosalts of the fahlore-group (tennantite, tetrahedrites and goldfieldite) and enargite-groups (enargite, luzonite, famatinite) found in the gold mineralization of the Gaching ore occurrence. The presence of Cu-rich and Se-bearing fahlores as well as enargite-group sulfosalts in ores indicate a high oxygen volatility at temperature less than 250° during their formation.

AB - The Gaching ore occurrence within the Maletoyvayam ore field is located in the southwestern part of Kamchatka volcanic belt. The ore occurrence belongs to high-sulfidation epithermal type. The sulfosalts of the fahlore-group (tennantite, tetrahedrites and goldfieldite) and enargite-groups (enargite, luzonite, famatinite) found in the gold mineralization of the Gaching ore occurrence. The presence of Cu-rich and Se-bearing fahlores as well as enargite-group sulfosalts in ores indicate a high oxygen volatility at temperature less than 250° during their formation.

KW - GOLDFIELDITE

KW - CHEMISTRY

KW - MINERALS

KW - RHODOPE

UR - http://www.scopus.com/inward/record.url?scp=85073059545&partnerID=8YFLogxK

U2 - 10.1088/1755-1315/319/1/012019

DO - 10.1088/1755-1315/319/1/012019

M3 - Conference article

AN - SCOPUS:85073059545

VL - 319

JO - IOP Conference Series: Earth and Environmental Science

JF - IOP Conference Series: Earth and Environmental Science

SN - 1755-1307

IS - 1

M1 - 012019

T2 - 10th All Russian Petrographic Conference with International Participationon Petrology of Magnetic and Metamorphic Complexes

Y2 - 27 November 2018 through 28 November 2018

ER -

ID: 21848554