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{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,9,16]],"date-time":"2024-09-16T16:14:02Z","timestamp":1726503242049},"reference-count":78,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[2010,1,1]],"date-time":"2010-01-01T00:00:00Z","timestamp":1262304000000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["SP"],"published-print":{"date-parts":[[2010,1]]},"abstract":"Abstract<\/jats:title>\n 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\u2013Akera suture zone; and (3) the Eurasian plate. Based on our field work, new stratigraphical, petrological, geochemical and geochronological data combined with previous data we present new insights on the subduction, obduction and collision processes recorded in the Lesser Caucasus. Two subductions are clearly identified, one related to the Neotethys subduction beneath the Eurasian margin and one intra-oceanic (SSZ) responsible for the opening of a back-arc basin which corresponds to the ophiolites of the Lesser Caucasus. The obduction occurred during the Late Coniacian to Santonian and is responsible for the widespread ophiolitic nappe outcrop in front of the suture zone. Following the subduction of oceanic lithosphere remnants under Eurasia, the collision of the SAB with Eurasia started during the Paleocene, producing 1) folding of ophiolites, arc and Upper Cretaceous formations (Transcaucasus massif to Karabakh); 2) thrusting toward SW; and 3) a foreland basin in front of the belt. Upper\u2013Middle Eocene series unconformably cover the three domains. From Eocene to Miocene as a result of the Arabian plate collision with the SAB to the South, southward propagation of shortening featured by folding and thrusting occurred all along the belt. These deformations are sealed by a thick sequence of unconformable Miocene to Quaternary clastic and volcanic rocks of debated origin.<\/jats:p>","DOI":"10.1144\/sp340.14","type":"journal-article","created":{"date-parts":[[2010,9,14]],"date-time":"2010-09-14T18:17:53Z","timestamp":1284488273000},"page":"329-352","source":"Crossref","is-referenced-by-count":122,"title":["Subductions, obduction and collision in the Lesser Caucasus (Armenia, Azerbaijan, Georgia), new insights"],"prefix":"10.1144","volume":"340","author":[{"given":"M.","family":"Sosson","sequence":"first","affiliation":[{"name":"Universit\u00e9 de Nice Sophia Antipolis, CNRS, OCA-UMR G\u00e9osciences Azur, 250 rue A. Einstein, Valbonne, France"}]},{"given":"Y.","family":"Rolland","sequence":"additional","affiliation":[{"name":"Universit\u00e9 de Nice Sophia Antipolis, CNRS, OCA-UMR G\u00e9osciences Azur, 250 rue A. Einstein, Valbonne, France"}]},{"given":"C.","family":"M\u00fcller","sequence":"additional","affiliation":[{"name":"6 bis rue Haute 92500 Rueil Malmaison, France"}]},{"given":"T.","family":"Danelian","sequence":"additional","affiliation":[{"name":"Universit\u00e9 de Lille, Laboratoire G\u00e9osyst\u00e8mes, FRE 3298, 59655 Villeneuve d'Ascq cedex, France"}]},{"given":"R.","family":"Melkonyan","sequence":"additional","affiliation":[{"name":"Institute of Geological Sciences, Armenian Academy of Sciences, 24 Baghramian ave, Yerevan, Armenia"}]},{"given":"S.","family":"Kekelia","sequence":"additional","affiliation":[{"name":"Institute of Geology, 1 M. Alexidze Street, 0193, Tbilisi, Georgia"}]},{"given":"S.","family":"Adamia","sequence":"additional","affiliation":[{"name":"Institute of Geophysics, 1 M. Alexidze Street, 0193, Tbilisi, Georgia"}]},{"given":"V.","family":"Babazadeh","sequence":"additional","affiliation":[{"name":"University of Baku, Baku, Azerbaijan"}]},{"given":"T.","family":"Kangarli","sequence":"additional","affiliation":[{"name":"Geological Institute of Azerbaijan, Geotectonics and Geodynamics, H.Javid Av., 29A, Baku AZ1143 Baku Azerbaijan"}]},{"given":"A.","family":"Avagyan","sequence":"additional","affiliation":[{"name":"Institute of Geological Sciences, Armenian Academy of Sciences, 24 Baghramian ave, Yerevan, Armenia"}]},{"given":"G.","family":"Galoyan","sequence":"additional","affiliation":[{"name":"Institute of Geological Sciences, Armenian Academy of Sciences, 24 Baghramian ave, Yerevan, Armenia"}]},{"given":"J.","family":"Mosar","sequence":"additional","affiliation":[{"name":"University of Friburg, Earth Sciences, Friburg, Switzerland"}]}],"member":"1881","published-online":{"date-parts":[[2010,9,3]]},"reference":[{"key":"e_1_3_2_2_1","first-page":"135","article-title":"Structure and development of the Loki salient of the Transcaucasus","volume":"1127","author":"Abesadze M.","year":"2002","unstructured":"Abesadze M., Adamia Sh., Chkhotua T., Tsimakuridze G., Shavishvili I.Structure and development of the Loki salient of the TranscaucasusProceedings, Geological Institute Academy of Sciences, Georgia, new series20021127135145(in Russian)","journal-title":"Proceedings, Geological Institute Academy of Sciences, Georgia, new series"},{"volume-title":"Geology and the Minerals (Ores) of the North-Eastern Coast of Sevan Lake","year":"1961","author":"Abovyan S. 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