Evolution of Rare-Metal Li–F Granite Melts in Sources of Ore-Magmatic Systems of Tigrinoe and Zabytoe Sn–W deposits (Central Sikhote-Alin, Primorye)

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Evolution of Rare-Metal Li–F Granite Melts in Sources of Ore-Magmatic Systems of Tigrinoe and Zabytoe Sn–W deposits (Central Sikhote-Alin, Primorye). / Gavryushkina, O. A.; Sokolova, E. N.; Smirnov, S. Z. et al.

In: Geology of Ore Deposits, Vol. 65, No. 6, 12.2023, p. 525-543.

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

BibTeX

@article{0b5afe2833584e48a7760db65cee39e2,

title = "Evolution of Rare-Metal Li–F Granite Melts in Sources of Ore-Magmatic Systems of Tigrinoe and Zabytoe Sn–W deposits (Central Sikhote-Alin, Primorye)",

abstract = "The present paper considers petrographic and geochemical features of rocks of the Tigrinoe and Zabytoe stocks, provides their mineral composition, the results of the detailed study of micas and mineral-forming inclusions in quartz. It is shown that the development of ore-magmatic systems (OMSs) of the Zabytoe and Tigrinoe deposits is associated with the same rare-metal Li–F melts. It is confirmed that granitoids of the Tigrinoe stock can be considered as more differentiated analogs of granitoids of the Zabytoe stock. New data concerning the differences in the history of the magmatic stage of development of the OMSs of these deposits are presented. The evolution of melts of both deposits took place at high fluid pressure. Differences in the scale of ore mineralization of the two RMSs under consideration could be due to different fluid regime of magmatic sources evolution and more significant participation of transmagmatic fluid flows in the development of the Tigrinoe OMS.",

keywords = "fluid inclusions, melt inclusions, mica, protolithionite, rare-metal granites, tin, tungsten, zinnwaldite",

author = "Gavryushkina, {O. A.} and Sokolova, {E. N.} and Smirnov, {S. Z.} and Kruk, {N. N.} and Ponomarchuk, {A. V.} and Tomas, {V. G.}",

note = "This work was supported by the Russian Foundation for Basic Research (project no. 20-05-00550) and performed within the framework of a state order to the Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences. Публикация для корректировки.",

year = "2023",

month = dec,

doi = "10.1134/S1075701523060041",

language = "English",

volume = "65",

pages = "525--543",

journal = "Geology of Ore Deposits",

issn = "1075-7015",

publisher = "Maik Nauka-Interperiodica Publishing",

number = "6",

}

RIS

TY - JOUR

T1 - Evolution of Rare-Metal Li–F Granite Melts in Sources of Ore-Magmatic Systems of Tigrinoe and Zabytoe Sn–W deposits (Central Sikhote-Alin, Primorye)

AU - Gavryushkina, O. A.

AU - Sokolova, E. N.

AU - Smirnov, S. Z.

AU - Kruk, N. N.

AU - Ponomarchuk, A. V.

AU - Tomas, V. G.

N1 - This work was supported by the Russian Foundation for Basic Research (project no. 20-05-00550) and performed within the framework of a state order to the Sobolev Institute of Geology and Mineralogy, Siberian Branch, Russian Academy of Sciences. Публикация для корректировки.

PY - 2023/12

Y1 - 2023/12

N2 - The present paper considers petrographic and geochemical features of rocks of the Tigrinoe and Zabytoe stocks, provides their mineral composition, the results of the detailed study of micas and mineral-forming inclusions in quartz. It is shown that the development of ore-magmatic systems (OMSs) of the Zabytoe and Tigrinoe deposits is associated with the same rare-metal Li–F melts. It is confirmed that granitoids of the Tigrinoe stock can be considered as more differentiated analogs of granitoids of the Zabytoe stock. New data concerning the differences in the history of the magmatic stage of development of the OMSs of these deposits are presented. The evolution of melts of both deposits took place at high fluid pressure. Differences in the scale of ore mineralization of the two RMSs under consideration could be due to different fluid regime of magmatic sources evolution and more significant participation of transmagmatic fluid flows in the development of the Tigrinoe OMS.

AB - The present paper considers petrographic and geochemical features of rocks of the Tigrinoe and Zabytoe stocks, provides their mineral composition, the results of the detailed study of micas and mineral-forming inclusions in quartz. It is shown that the development of ore-magmatic systems (OMSs) of the Zabytoe and Tigrinoe deposits is associated with the same rare-metal Li–F melts. It is confirmed that granitoids of the Tigrinoe stock can be considered as more differentiated analogs of granitoids of the Zabytoe stock. New data concerning the differences in the history of the magmatic stage of development of the OMSs of these deposits are presented. The evolution of melts of both deposits took place at high fluid pressure. Differences in the scale of ore mineralization of the two RMSs under consideration could be due to different fluid regime of magmatic sources evolution and more significant participation of transmagmatic fluid flows in the development of the Tigrinoe OMS.

KW - fluid inclusions

KW - melt inclusions

KW - mica

KW - protolithionite

KW - rare-metal granites

KW - tin

KW - tungsten

KW - zinnwaldite

UR - https://www.scopus.com/record/display.uri?eid=2-s2.0-85181672723&origin=inward&txGid=f844ca77cd1ea7a1e27ec5b1e12011b5

UR - https://www.mendeley.com/catalogue/c79cd908-cf99-35a8-8aba-64e9012c56fc/

U2 - 10.1134/S1075701523060041

DO - 10.1134/S1075701523060041

M3 - Article

VL - 65

SP - 525

EP - 543

JO - Geology of Ore Deposits

JF - Geology of Ore Deposits

SN - 1075-7015

IS - 6

ER -

ID: 59543901