University of Côte d'Azur
Status: Research institution
Email jedi-innovation@univ-cotedazur.fr
Website http://univ-cotedazur.fr/fr
Address Welcome Center 24 avenue des Diables Bleus Bât ISEM - bureau 232 06300 Nice , Nice , France,
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Bibliography
Caucasus collisional history: Review of data from East Anatolia to West Iran
A review of the plate convergence history of the East Anatolia-Transcaucasus region during the Variscan: Insights from the Georgian basement and its connection to the Eastern Pontides
Evidence for ∼80–75Ma subduction jump during Anatolide–Tauride–Armenian block accretion and ∼48Ma Arabia–Eurasia collision in Lesser Caucasus–East Anatolia
Prolonged Variscan to Alpine history of an active Eurasian margin (Georgia, Armenia) revealed by 40Ar/39Ar dating
What is the lithological nature of subduction channels? Insights from fossil Caucasus subduction zones
The Armenian Ophiolite: Insights for Jurassic back-arc formation, Lower Cretaceous hot spot magmatism and Upper Cretaceous obduction over the South Armenian Block
Blueschists of the Amassia-Stepanavan Suture Zone (Armenia):linking Tethys subduction history from E-Turkey to W-Iran
Obduction of old oceanic lithosphere due to reheating and plate reorganization: Insights from numerical modelling and the NE Anatolia - Lesser Caucasus case example
Lithological nature of the Subduction Channel: Insights from the Karabakh suture zone (Lesser Caucasus) and general comparisons
The Armenian and NW Anatolian ophiolites: new insights for the closure of the Tethys domain and obduction onto the South Armenian Block and Anatolian-Tauride Platform before collision through dynamic modeling
New P-T-t data on the metamorphic sole of the Amasia ophiolites and implications for the geodynamical process, NW of the Sevan-Akera suture zone, Lesser Caucasus (Armenia)
Insights on the lithological nature of subduction channels from observations of fossil subduction zones, Sevan-Akera suture zone, Lesser Caucasus (Armenia and Karabakh)
Geology and Structure of the Amasia Ophiolites, NW of the Sevan-Akera Suture Zone, Lesser Caucasus (Armenia)
New structural and petrological data on the Amasia ophiolites (NW Sevan-Akera suture zone, Lesser Caucasus): Insights for a larg-scale obduction in Armenia and NE Turkey.
From seafloor spreading to obduction: Jurassic–Cretaceous evolution of the northern branch of the Neotethys in the Northeastern Anatolian and Lesser Caucasus regions
From Subduction to Obduction: new insights on the obduction process through the study of the metamorphic sole of the Amasia ophiolites (Lesser Caucasus, Armenia)
Large scale obduction of preserved oceanic crust: linking the Lesser Caucasus and NE Anatolian ophiolites and implications for the formation of the Lesser Caucasus-Pontides Arc
Linking the NE Anatolian and Lesser Caucasus ophiolites: Evidence for large-scale obduction of oceanic crust and implications for the formation of the Lesser Caucasus-Pontides Arc
Obduction triggered by regional heating during plate reorganization
OBDUCTION IN NE ANATOLIA AND LESSER CAUCASUS REGIONS: EMPLACEMENT OF OLD OCEANIC LITHOSPHERE (80 MA), GEOLOGIC CONSTRAINTS AND INPUT FROM NUMERICAL MODELLING
Multi-stage metamorphism in the South Armenian Block during the Late Jurassic to Early Cretaceous: Tectonics over south-dipping subduction of Northern branch of Neotethys
The East Anatolia-Lesser Caucasus ophiolite: An exceptional case of large-scale obduction, synthesis of data and numerical modelling