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Konstantinos Papapavlou

Université du Québec à Montréal

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Craig Storey

University of Portsmouth

James Darling

University of Portsmouth

D. E. Moser

Western University

Abdelali Moukhsil

Ministry of Natural Resources and Wildlife

Stéphanie Lasalle

University of Portsmouth

Peter C. Lightfoot

Western University

D. Bullen

University of Portsmouth

André Poirier

Université du Québec à Montréal

Nikolaos Gerogiannis

University of Patras

Eirini Aravadinou

University of Patras

Cooperative Institutions

University of Portsmouth

University of Toronto

Western University

University of Patras

The Open University

Université du Québec à Montréal

University of Wisconsin–Madison

Vale (Canada)

University of Minnesota

Twin Cities Orthopedics

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THE ACCRETIONARY GROWTH AND REWORKING OF SOUTHEASTERN LAURENTIA THROUGH THE U-PB-HF DETRITAL ZIRCON RECORD: INSIGHTS FROM THE LAC-SAINT-JEAN REGION (CENTRAL GRENVILLE PROVINCE, QUEBEC, CA)

Abstracts with programs - Geological Society of America (2020)

Konstantinos Papapavlou Abdelali Moukhsil André Poirier

Laurentia

10.1130/abs/2020am-350542

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Deformation within the Cycladic subduction–exhumation channel: new insights from the enigmatic Makrotantalo nappe (Andros, Aegean)

International Journal of Earth Sciences (2019)

Nikolaos Gerogiannis P. Xypolias Vasileios Chatzaras Eirini Aravadinou Konstantinos Papapavlou

Blueschist

CYCLADES

Glaucophane

Tectonic phase

10.1007/s00531-019-01680-3

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Citations (21)

Zircon U–Pb–Hf snapshots on the crustal evolution of the Serbo-Macedonian massif: new insights from Ammouliani island (Northern Greece)

Geological Magazine (2021)

Konstantinos Papapavlou

Abstract Zircon U–Pb and Lu–Hf isotope microanalysis was conducted in (meta)-igneous units of Ammouliani island to characterize crust-forming and reworking events in the Serbo-Macedonian massif. Zircon grains from an orthogneiss of the Vertiskos unit yielded a U–Pb crystallization age for the igneous precursor at 458.8 ± 11 Ma with dominantly subchondritic ϵHf values indicating reworking of Neoproterozoic basement. A weighted mean ϵHf value of 0.7 ± 2.4 from oscillatory zoned zircon grains of the Ouranoupoli granodiorite indicates juvenile crustal input at 52.1 ± 0.6 Ma. The U–Pb–Hf zircon archive records discrete stages in the crustal evolution of the Serbo-Macedonian massif.

Massif

Macedonian

Basement

10.1017/s0016756821000698

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Citations (2)