Similar geological, petrological, geochemical and age features are found in various Armenian ophiolitic massifs (Sevan, Stepanavan and Vedi). These data argue for the presence of a single large ophiolite unit obducted on the South Armenian Block (SAB). Lherzolite Ophiolite type rock assemblages evidence a Lower–Middle Jurassic slow-spreading...
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2010 (v1)Book sectionUploaded on: December 3, 2022
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2007 (v1)Journal article
Comptes Rendus Géoscience, v. 339, n. 7, p. 482-492, 2007. http://dx.doi.org/10.1016/j.crte.2007.06.002
Uploaded on: December 3, 2022 -
2009 (v1)Journal article
Journal of Asian Earth Sciences, v. 34, n. 2, p. 135153, 2009. http://dx.doi.org/10.1016/j.jseaes.2008.04.002
Uploaded on: December 3, 2022 -
2005 (v1)Journal article
Geodinamica Acta, v. 18, n. 6, p. 401-416, 2005. http://dx.doi.org/10.3166/ga.18.401-416
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2010 (v1)Book section
The stress indicators describing the recent (provided by active tectonics framework) and palaeo-stress (provided by micro-fault kinematics and volcanic cluster) patterns show the scale and temporal changes in stress states since the beginning of Arabian–Eurasian collision. The recent stress derived from the active fault kinematics in the Lesser...
Uploaded on: December 3, 2022 -
2010 (v1)Book section
In the Lesser Caucasus three main domains are distinguished from SW to NE: (1) the autochthonous South Armenian Block (SAB), a Gondwana-derived terrane; (2) the ophiolitic Sevan–Akera suture zone; and (3) the Eurasian plate. Based on our field work, new stratigraphical, petrological, geochemical and geochronological data combined with previous...
Uploaded on: December 3, 2022