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Late Permian high-pressure metamorphism in the Devesil Unit, East Rhodopes (SE Bulgaria) – Single or multiple metamorphic events. / Macheva, Lyubomirka ; Machev, Philip ; Peytcheva, Irena ; Guillong, Marcel ; Plotkina, Julia ; Salnikova, Еkaterina ; Koreshkova, Marina .

In: Review of the Bulgarian Geological Society, Vol. 83, No. 3, 2022, p. 109-112.

Research output: Contribution to journal › Conference article › peer-review

Harvard

Macheva, L, Machev, P, Peytcheva, I, Guillong, M, Plotkina, J, Salnikova, Е & Koreshkova, M 2022, 'Late Permian high-pressure metamorphism in the Devesil Unit, East Rhodopes (SE Bulgaria) – Single or multiple metamorphic events', Review of the Bulgarian Geological Society, vol. 83, no. 3, pp. 109-112. https://doi.org/10.52215/rev.bgs.2022.83.3.109, https://doi.org/DOI: 10.52215/rev.bgs.2022.83.3.109

APA

Macheva, L., Machev, P., Peytcheva, I., Guillong, M., Plotkina, J., Salnikova, Е., & Koreshkova, M. (2022). Late Permian high-pressure metamorphism in the Devesil Unit, East Rhodopes (SE Bulgaria) – Single or multiple metamorphic events. Review of the Bulgarian Geological Society, 83(3), 109-112. https://doi.org/10.52215/rev.bgs.2022.83.3.109, https://doi.org/DOI: 10.52215/rev.bgs.2022.83.3.109

Vancouver

Macheva L, Machev P, Peytcheva I, Guillong M, Plotkina J, Salnikova Е et al. Late Permian high-pressure metamorphism in the Devesil Unit, East Rhodopes (SE Bulgaria) – Single or multiple metamorphic events. Review of the Bulgarian Geological Society. 2022;83(3):109-112. https://doi.org/10.52215/rev.bgs.2022.83.3.109, https://doi.org/DOI: 10.52215/rev.bgs.2022.83.3.109

Author

Macheva, Lyubomirka ; Machev, Philip ; Peytcheva, Irena ; Guillong, Marcel ; Plotkina, Julia ; Salnikova, Еkaterina ; Koreshkova, Marina . / Late Permian high-pressure metamorphism in the Devesil Unit, East Rhodopes (SE Bulgaria) – Single or multiple metamorphic events. In: Review of the Bulgarian Geological Society. 2022 ; Vol. 83, No. 3. pp. 109-112.

BibTeX

@article{1e11de92fbd247ac9e3cabe4c9eca931,
title = "Late Permian high-pressure metamorphism in the Devesil Unit, East Rhodopes (SE Bulgaria) – Single or multiple metamorphic events",
abstract = "Metaeclogites from the Devesil Unit, East Rhodopes are studied. Well preserved eclogite paragenesis is presented by omphacite+garnet+rutile and is obliterated by still high temperature retrograde assemblage of newly formed garnet, diopside, amphibole, plagioclase, titanite, and quartz. The P-T conditions of the high pressure metamor-phism are in the range 620–665 °C and 1.8–2.0 GPa, whereas the retrograde stage occurs at temperature 600–650 °C and pressure 0.6–0,8 GPa. Cathodoluminescence images and LA-ICP-MS dating of zircon grains point to multiple metamorphic origin of the mineral the earliest with Late Permian–Early Triassic age, followed by Early Jurassic and Early Cretaceous metamorphic events",
keywords = "East Rhodopes, metamorphism, eclogites, zircon",
author = "Lyubomirka Macheva and Philip Machev and Irena Peytcheva and Marcel Guillong and Julia Plotkina and Еkaterina Salnikova and Marina Koreshkova",
year = "2022",
doi = "10.52215/rev.bgs.2022.83.3.109",
language = "English",
volume = "83",
pages = "109--112",
journal = "Review of the Bulgarian Geological Society",
issn = "0007-3938",
number = "3",

}

RIS

TY - JOUR

T1 - Late Permian high-pressure metamorphism in the Devesil Unit, East Rhodopes (SE Bulgaria) – Single or multiple metamorphic events

AU - Macheva, Lyubomirka

AU - Machev, Philip

AU - Peytcheva, Irena

AU - Guillong, Marcel

AU - Plotkina, Julia

AU - Salnikova, Еkaterina

AU - Koreshkova, Marina

PY - 2022

Y1 - 2022

N2 - Metaeclogites from the Devesil Unit, East Rhodopes are studied. Well preserved eclogite paragenesis is presented by omphacite+garnet+rutile and is obliterated by still high temperature retrograde assemblage of newly formed garnet, diopside, amphibole, plagioclase, titanite, and quartz. The P-T conditions of the high pressure metamor-phism are in the range 620–665 °C and 1.8–2.0 GPa, whereas the retrograde stage occurs at temperature 600–650 °C and pressure 0.6–0,8 GPa. Cathodoluminescence images and LA-ICP-MS dating of zircon grains point to multiple metamorphic origin of the mineral the earliest with Late Permian–Early Triassic age, followed by Early Jurassic and Early Cretaceous metamorphic events

AB - Metaeclogites from the Devesil Unit, East Rhodopes are studied. Well preserved eclogite paragenesis is presented by omphacite+garnet+rutile and is obliterated by still high temperature retrograde assemblage of newly formed garnet, diopside, amphibole, plagioclase, titanite, and quartz. The P-T conditions of the high pressure metamor-phism are in the range 620–665 °C and 1.8–2.0 GPa, whereas the retrograde stage occurs at temperature 600–650 °C and pressure 0.6–0,8 GPa. Cathodoluminescence images and LA-ICP-MS dating of zircon grains point to multiple metamorphic origin of the mineral the earliest with Late Permian–Early Triassic age, followed by Early Jurassic and Early Cretaceous metamorphic events

KW - East Rhodopes

KW - metamorphism

KW - eclogites

KW - zircon

UR - https://www.researchgate.net/publication/366512616_Late_Permian_high-pressure_metamorphism_in_the_Devesil_Unit_East_Rhodopes_SE_Bulgaria_-_Single_or_multiple_metamorphic_events

U2 - 10.52215/rev.bgs.2022.83.3.109

DO - 10.52215/rev.bgs.2022.83.3.109

M3 - Conference article

VL - 83

SP - 109

EP - 112

JO - Review of the Bulgarian Geological Society

JF - Review of the Bulgarian Geological Society

SN - 0007-3938

IS - 3

ER -

ID: 102621511