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The First Finding of Sapphirine in Granulites of the Angara–Kan Block : Evidence of Ultra-High–Temperature Metamorphism in the SW Siberian Craton. / Sukhorukov, V. P.; Gladkochub, D. P.; Turkina, O. M.

в: Doklady Earth Sciences, Том 479, № 2, 01.04.2018, стр. 443-447.

Результаты исследований: Научные публикации в периодических изданиях › статья › Рецензирование

Harvard

Sukhorukov, VP, Gladkochub, DP & Turkina, OM 2018, 'The First Finding of Sapphirine in Granulites of the Angara–Kan Block: Evidence of Ultra-High–Temperature Metamorphism in the SW Siberian Craton', Doklady Earth Sciences, Том. 479, № 2, стр. 443-447. https://doi.org/10.1134/S1028334X18040190

APA

Sukhorukov, V. P., Gladkochub, D. P., & Turkina, O. M. (2018). The First Finding of Sapphirine in Granulites of the Angara–Kan Block: Evidence of Ultra-High–Temperature Metamorphism in the SW Siberian Craton. Doklady Earth Sciences, 479(2), 443-447. https://doi.org/10.1134/S1028334X18040190

Vancouver

Sukhorukov VP, Gladkochub DP, Turkina OM. The First Finding of Sapphirine in Granulites of the Angara–Kan Block: Evidence of Ultra-High–Temperature Metamorphism in the SW Siberian Craton. Doklady Earth Sciences. 2018 апр. 1;479(2):443-447. doi: 10.1134/S1028334X18040190

Author

Sukhorukov, V. P. ; Gladkochub, D. P. ; Turkina, O. M. / The First Finding of Sapphirine in Granulites of the Angara–Kan Block : Evidence of Ultra-High–Temperature Metamorphism in the SW Siberian Craton. в: Doklady Earth Sciences. 2018 ; Том 479, № 2. стр. 443-447.

BibTeX

@article{e03de7d6bdae40b0a9d7995b279dbef4,
title = "The First Finding of Sapphirine in Granulites of the Angara–Kan Block: Evidence of Ultra-High–Temperature Metamorphism in the SW Siberian Craton",
abstract = "This work reports the first discovery of sapphirine-bearing mineral parageneses in granulites of the Angara–Kan block, information on the mineral assemblage of rocks, and the mineral composition. Based on mineral geothermometers utilizing alumina content in orthopyroxene, reconstruction of the composition of ternary feldspar, and the titanium content in zircon, it was revealed that the peak temperatures of metamorphism reached 1100°C, after which the rocks underwent cooling under sub-isobaric conditions. It is assumed that the pulse of ultra-high-temperature metamorphism correlates with processes of extension and intraplate magmatism during the age interval of 1.78–1.75 Ga.",
keywords = "CRUSTAL METAMORPHISM, UHT METAMORPHISM, NAPIER COMPLEX, THERMOMETRY, ANTARCTICA",
author = "Sukhorukov, {V. P.} and Gladkochub, {D. P.} and Turkina, {O. M.}",
year = "2018",
month = apr,
day = "1",
doi = "10.1134/S1028334X18040190",
language = "English",
volume = "479",
pages = "443--447",
journal = "Doklady Earth Sciences",
issn = "1028-334X",
publisher = "PLEIADES PUBLISHING INC",
number = "2",

}

RIS

TY - JOUR

T1 - The First Finding of Sapphirine in Granulites of the Angara–Kan Block

T2 - Evidence of Ultra-High–Temperature Metamorphism in the SW Siberian Craton

AU - Sukhorukov, V. P.

AU - Gladkochub, D. P.

AU - Turkina, O. M.

PY - 2018/4/1

Y1 - 2018/4/1

N2 - This work reports the first discovery of sapphirine-bearing mineral parageneses in granulites of the Angara–Kan block, information on the mineral assemblage of rocks, and the mineral composition. Based on mineral geothermometers utilizing alumina content in orthopyroxene, reconstruction of the composition of ternary feldspar, and the titanium content in zircon, it was revealed that the peak temperatures of metamorphism reached 1100°C, after which the rocks underwent cooling under sub-isobaric conditions. It is assumed that the pulse of ultra-high-temperature metamorphism correlates with processes of extension and intraplate magmatism during the age interval of 1.78–1.75 Ga.

AB - This work reports the first discovery of sapphirine-bearing mineral parageneses in granulites of the Angara–Kan block, information on the mineral assemblage of rocks, and the mineral composition. Based on mineral geothermometers utilizing alumina content in orthopyroxene, reconstruction of the composition of ternary feldspar, and the titanium content in zircon, it was revealed that the peak temperatures of metamorphism reached 1100°C, after which the rocks underwent cooling under sub-isobaric conditions. It is assumed that the pulse of ultra-high-temperature metamorphism correlates with processes of extension and intraplate magmatism during the age interval of 1.78–1.75 Ga.

KW - CRUSTAL METAMORPHISM

KW - UHT METAMORPHISM

KW - NAPIER COMPLEX

KW - THERMOMETRY

KW - ANTARCTICA

UR - http://www.scopus.com/inward/record.url?scp=85047260664&partnerID=8YFLogxK

U2 - 10.1134/S1028334X18040190

DO - 10.1134/S1028334X18040190

M3 - Article

AN - SCOPUS:85047260664

VL - 479

SP - 443

EP - 447

JO - Doklady Earth Sciences

JF - Doklady Earth Sciences

SN - 1028-334X

IS - 2

ER -

ID: 13488327