P–T CONDITIONS, U/Pb AND 40Ar/39Ar ISOTOPIC AGES OF UHT GRANULITES FROM CAPE KALTYGEI, WESTERN BAIKAL REGION

The study is focused on metapelitic granulites of Cape Kaltygei (Western Baikal region) that contain a diagnostic mineral assemblage of ultrahigh temperature (UHT) metamorphic rocks (orthopyroxene+sillimanite+quartz). The pseudosection-based thermobarometry yields peak metamorphic temperature and pr...

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Main Authors: N. I. Volkova, E. I. Mikheev, A. V. Travin, A. G. Vladimirov, A. S. Mekhonoshin, V. V. Khlestov
Format: Article
Language:English
Published: Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust 2021-06-01
Series:Геодинамика и тектонофизика
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Online Access:https://www.gt-crust.ru/jour/article/view/1213
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author N. I. Volkova
E. I. Mikheev
A. V. Travin
A. G. Vladimirov
A. S. Mekhonoshin
V. V. Khlestov
author_facet N. I. Volkova
E. I. Mikheev
A. V. Travin
A. G. Vladimirov
A. S. Mekhonoshin
V. V. Khlestov
author_sort N. I. Volkova
collection DOAJ
description The study is focused on metapelitic granulites of Cape Kaltygei (Western Baikal region) that contain a diagnostic mineral assemblage of ultrahigh temperature (UHT) metamorphic rocks (orthopyroxene+sillimanite+quartz). The pseudosection-based thermobarometry yields peak metamorphic temperature and pressure values (T=950 °C, P=~9 kbar) and suggests near-isobaric cooling (IBC) conditions during the retrograde evolution of the granulites. The U/Pb zircon age estimates for metamorphism (~1.87 Ga) support the data published by other researchers. The SHRIMP-II U-Pb dating of zircon cores yields a minimum protolith age of 1.94–1.91 Ga. Biotites and amphiboles from granulites of Cape Kaltygei show the 40Ar/39Ar isotopic ages that are close to the Early Paleozoic accretion-collision system of the Western Baikal region.
format Article
id doaj-art-2cadf74cf59c4d0ea9aef6893e9c0054
institution Kabale University
issn 2078-502X
language English
publishDate 2021-06-01
publisher Russian Academy of Sciences, Siberian Branch, Institute of the Earth's crust
record_format Article
series Геодинамика и тектонофизика
spelling doaj-art-2cadf74cf59c4d0ea9aef6893e9c00542025-08-20T03:37:06ZengRussian Academy of Sciences, Siberian Branch, Institute of the Earth's crustГеодинамика и тектонофизика2078-502X2021-06-0112231033110.5800/GT-2021-12-2-0526527P–T CONDITIONS, U/Pb AND 40Ar/39Ar ISOTOPIC AGES OF UHT GRANULITES FROM CAPE KALTYGEI, WESTERN BAIKAL REGIONN. I. Volkova0E. I. Mikheev1A. V. Travin2A. G. Vladimirov3A. S. Mekhonoshin4V. V. Khlestov5Sobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesSobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences; Novosibirsk State UniversitySobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences; Novosibirsk State University; Tomsk State UniversitySobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of Sciences; Tomsk State UniversityVinogradov Institute of Geochemistry, Siberian Branch of the Russian Academy of Sciences; Irkutsk National Research Technical UniversitySobolev Institute of Geology and Mineralogy, Siberian Branch of the Russian Academy of SciencesThe study is focused on metapelitic granulites of Cape Kaltygei (Western Baikal region) that contain a diagnostic mineral assemblage of ultrahigh temperature (UHT) metamorphic rocks (orthopyroxene+sillimanite+quartz). The pseudosection-based thermobarometry yields peak metamorphic temperature and pressure values (T=950 °C, P=~9 kbar) and suggests near-isobaric cooling (IBC) conditions during the retrograde evolution of the granulites. The U/Pb zircon age estimates for metamorphism (~1.87 Ga) support the data published by other researchers. The SHRIMP-II U-Pb dating of zircon cores yields a minimum protolith age of 1.94–1.91 Ga. Biotites and amphiboles from granulites of Cape Kaltygei show the 40Ar/39Ar isotopic ages that are close to the Early Paleozoic accretion-collision system of the Western Baikal region.https://www.gt-crust.ru/jour/article/view/1213cape kaltygeiwestern baikal regionuht granulitesp–t pseudosectionsu-pb and ar-ar geochronology
spellingShingle N. I. Volkova
E. I. Mikheev
A. V. Travin
A. G. Vladimirov
A. S. Mekhonoshin
V. V. Khlestov
P–T CONDITIONS, U/Pb AND 40Ar/39Ar ISOTOPIC AGES OF UHT GRANULITES FROM CAPE KALTYGEI, WESTERN BAIKAL REGION
Геодинамика и тектонофизика
cape kaltygei
western baikal region
uht granulites
p–t pseudosections
u-pb and ar-ar geochronology
title P–T CONDITIONS, U/Pb AND 40Ar/39Ar ISOTOPIC AGES OF UHT GRANULITES FROM CAPE KALTYGEI, WESTERN BAIKAL REGION
title_full P–T CONDITIONS, U/Pb AND 40Ar/39Ar ISOTOPIC AGES OF UHT GRANULITES FROM CAPE KALTYGEI, WESTERN BAIKAL REGION
title_fullStr P–T CONDITIONS, U/Pb AND 40Ar/39Ar ISOTOPIC AGES OF UHT GRANULITES FROM CAPE KALTYGEI, WESTERN BAIKAL REGION
title_full_unstemmed P–T CONDITIONS, U/Pb AND 40Ar/39Ar ISOTOPIC AGES OF UHT GRANULITES FROM CAPE KALTYGEI, WESTERN BAIKAL REGION
title_short P–T CONDITIONS, U/Pb AND 40Ar/39Ar ISOTOPIC AGES OF UHT GRANULITES FROM CAPE KALTYGEI, WESTERN BAIKAL REGION
title_sort p t conditions u pb and 40ar 39ar isotopic ages of uht granulites from cape kaltygei western baikal region
topic cape kaltygei
western baikal region
uht granulites
p–t pseudosections
u-pb and ar-ar geochronology
url https://www.gt-crust.ru/jour/article/view/1213
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