Researcher interests: Tectonics of orogenic belts, with emphasis on the Western Alps and the Aegean region. Extensional tectonics and the origin of Mediterranean back-arc basins. Crustal evolution of the Arabo-Nubian shield. The detrital record of orogeny. Neoproterozoic-Cambr
FACULTY / SCHOOL: Faculty of Science
DEPARTMENT: The Institute of Earth Sciences
Selected Publications
crustal evolution of peri gondwana crust into present day europe the serbo macedonian and rhodope massifs as a case study (2019)|
Lithos|
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from peri gondwana to present day europe crustal evolution of the balkan as a case study for the continent (2019)|
GSA Annual Meeting in Phoenix, Arizona, USA - 2019|
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provenance of the great cambrian sandstone succession of northern gondwana unravelled by strontium neodymium and lead isotopes of feldspars and clays (2018)|
Sedimentology|
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new detrital zircon geochronology from the cycladic basement greece implications for the paleozoic accretion of peri gondwanan terranes to laurussia (2018)|
Tectonics|
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the lower crust of the northern broken edge of gondwana evidence for sediment subduction and syn variscan anorogenic imprint from zircon u pb hf in granulite xenoliths (2018)|
Gondwana Research|
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cadomian metasediments and ordovician sandstone from corsica detrital zircon u pb hf constrains on their provenance and paleogeography (2018)|
International Journal of Earth Sciences|
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the white nile as a source for nile sediments assessment using u pb geochronology of detrital rutile and monazite (2018)|
Journal of African Earth Sciences|
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detrital rutile u pb perspective on the origin of the great cambro ordovician sandstone of north gondwana and its linkage to orogeny (2017)|
Gondwana Research|
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the pelagonian terrane of greece in the peri gondwanan mosaic of the eastern mediterranean implications for the geological evolution of avalonia (2017)|
Precambrian Research|
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origin of the eastern mediterranean neotethys rifting along a cryptic cadomian suture with afro arabia (2016)|
Geological Society of America Bulletin|
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