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U-Th-He geochronology of pyrite from the uzelga VMS deposit (South urals)—new perspectives for direct dating of the ore-forming processes. / Yakubovich, Olga; Podolskaya, Mary; Vikentyev, Ilya; Fokina, Elena; Kotov, Alexander.
в: Minerals, Том 10, № 7, 629, 07.2020, стр. 1-20.Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование
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TY - JOUR
T1 - U-Th-He geochronology of pyrite from the uzelga VMS deposit (South urals)—new perspectives for direct dating of the ore-forming processes
AU - Yakubovich, Olga
AU - Podolskaya, Mary
AU - Vikentyev, Ilya
AU - Fokina, Elena
AU - Kotov, Alexander
PY - 2020/7
Y1 - 2020/7
N2 - We report on the application of the U-Th-He method for the direct dating of pyrite and provide an original methodological approach for measurement of U, Th and He in single grains without loss of parent nuclides during thermal extraction of He. The U-Th-He age of ten samples of high-crystalline stoichiometric pyrite from unoxidized massive ores of the Uzelga volcanogenic massive sulfide (VMS) deposit, South Urals, is 382 ± 12 Ma (2σ) (U concentrations ~1–5 ppm;4 He ~10−4 cm3 STP g−1). This age is consistent with independent (biostratigraphic) estimations of the age of ore formation (ca, 389–380 Ma) and is remarkably older than the probable age of the regional prehnite-pumpellyite facies metamorphism (~340–345 Ma). Our results indicate that the U-Th-He dating of ~1 mg weight pyrite sample is possible and open new perspectives for the dating of ore deposits. The relative simplicity of U-Th-He dating in comparison with other geochronological methods makes this approach interesting for further application.
AB - We report on the application of the U-Th-He method for the direct dating of pyrite and provide an original methodological approach for measurement of U, Th and He in single grains without loss of parent nuclides during thermal extraction of He. The U-Th-He age of ten samples of high-crystalline stoichiometric pyrite from unoxidized massive ores of the Uzelga volcanogenic massive sulfide (VMS) deposit, South Urals, is 382 ± 12 Ma (2σ) (U concentrations ~1–5 ppm;4 He ~10−4 cm3 STP g−1). This age is consistent with independent (biostratigraphic) estimations of the age of ore formation (ca, 389–380 Ma) and is remarkably older than the probable age of the regional prehnite-pumpellyite facies metamorphism (~340–345 Ma). Our results indicate that the U-Th-He dating of ~1 mg weight pyrite sample is possible and open new perspectives for the dating of ore deposits. The relative simplicity of U-Th-He dating in comparison with other geochronological methods makes this approach interesting for further application.
KW - Geochronology
KW - Helium dating
KW - Pyrite
KW - Uzelga
KW - VMS deposits
UR - http://www.scopus.com/inward/record.url?scp=85088045755&partnerID=8YFLogxK
U2 - 10.3390/min10070629
DO - 10.3390/min10070629
M3 - Article
AN - SCOPUS:85088045755
VL - 10
SP - 1
EP - 20
JO - Minerals
JF - Minerals
SN - 2075-163X
IS - 7
M1 - 629
ER -
ID: 61033691