Protolithic age and time of metamorphism of amphibolites from Slasten lithotectonic unit (Southern Pirin Mountains)

The investigated amphibolites from the Slasten lithotectonic unit are found as a strongly elongated body trending north-south at the eastern slope of the Pirin Mountain, near the village of Ilinden. These rocks are hosted by biotite and biotite-amphibole gneisses, some partially migmatized and containing thin intercalations of marble. The mineral composition is amphibole, plagioclase, epidote, quartz, garnet, pyroxene, titanite, and calcite. P-T conditions of metamorphism are in the range 691–724°C and 0.74–0.86 GPa. LA-ICP-MS analyses of zircons yield a Middle Triassic (246.4±3.2 Ma) age of formation of these amphibolites.

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Publication Details

Journal
Review of the Bulgarian Geological Society
Published
2024-11-01
DOI
https://doi.org/10.52215/rev.bgs.2024.85.2.183
Primary Topic
Geological Formations and Processes Exploration
Type
article
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article

Protolithic age and time of metamorphism of amphibolites from Slasten lithotectonic unit (Southern Pirin Mountains)

Philip Machev, Lyubomirka Macheva, Irena Peytcheva, М. В. Стифеева et al.
Review of the Bulgarian Geological Society
Geological Formations and Processes Exploration
article

Protolithic age and time of metamorphism of amphibolites from Slasten lithotectonic unit (Southern Pirin Mountains)

Philip Machev, Lyubomirka Macheva, Irena Peytcheva, М. В. Стифеева, Е. Б. Сальникова, Julia Plotkina
article en

Abstract

The investigated amphibolites from the Slasten lithotectonic unit are found as a strongly elongated body trending north-south at the eastern slope of the Pirin Mountain, near the village of Ilinden. These rocks are hosted by biotite and biotite-amphibole gneisses, some partially migmatized and containing thin intercalations of marble. The mineral composition is amphibole, plagioclase, epidote, quartz, garnet, pyroxene, titanite, and calcite. P-T conditions of metamorphism are in the range 691–724°C and 0.74–0.86 GPa. LA-ICP-MS analyses of zircons yield a Middle Triassic (246.4±3.2 Ma) age of formation of these amphibolites.

Review of the Bulgarian Geological SocietyVol. 85(2)
Openalex Percentile: Top 77%
Geological Formations and Processes Exploration
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