Albania is part of the Dinaride-Albanid-Hellenic are of Alpine orogeny. The collision of the African and Euroasian plates caused the Albanides to become folded and displaced from the east to the west....
The Mirdita Ophiolite forms the northern Albanian segment of this unit. In northeast Albania near Bajram Curri, a 200–700 m thick metamorphic sole is preserved at its base.
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To better understand interrelated tectonometamorphic and hydraulic processes associated with incipient intraoceanic subduction, we mapped c. 65 km^2 along a well-preserved subduction
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The Mirdita Ophiolite forms the northern Albanian segment of this unit. In northeast Albania near Bajram Curri, a 200–700 m thick metamorphic sole is
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To better understand interrelated tectonometamorphic and hydraulic processes associated with incipient intraoceanic subduction, we mapped c. 65
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This Plan is designed to reduce the socio-economic gap between Albania and EU Member States by driving modernisation and digitalisation, strengthening Albania''s economy and
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The external thrustbelt of Albania consists of some tectonic zones (Ionian, Kruja and Krasta-Cukali zones), that are westward overthrust, with a large amplitude (50e100 km), above the Apulian
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Carbon Capture and Storage Regulation has to be transposed as Albania has some geology potential and thus should consider introducing some potential permitting system.
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Frontal accretion of oceanic sediments as well as passive continental nappe-transport are late stage phases. To study these processes linked to subduction, we mapped ~35 km2 of the
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Frontal accretion of oceanic sediments as well as passive continental nappe-transport are late stage phases. To study these processes linked to
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During the Neogene''s the northwards movement of the African Plate, enhanced compression, leading to a large scale folding and thrusting in the SW direction in Albania and NW of Greece.
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The assembly of obducted mantle rocks and metamorphic sole constitutes a plate interface that formed during the intraoceanic subduction stage preceding obduction; we call this a fossil intraoceanic plate
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In north-eastern Albania, the plate interface exposes a metamorphic sole below foliated and serpentinised harzburgites and is therefore a perfect laboratory to study the interplay of
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