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{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,9,16]],"date-time":"2024-09-16T20:36:33Z","timestamp":1726518993796},"reference-count":67,"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 \n 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\u2013Middle Jurassic slow-spreading rate. The lavas and gabbros have a hybrid geochemical composition intermediate between arc and Mid Ocean Ridge Basalt (MORB) signatures which suggest they were probably formed in a back-arc basin. This oceanic sequence is overlain by pillowed alkaline lavas emplaced in marine conditions. Their geochemical composition is similar to plateau-lavas. Finally, this thickened oceanic crust is overlain by Upper Cretaceous calc-alkaline lavas likely formed in a supra-subduction zone environment. The age of the ophiolite is constrained by\n 40<\/jats:sup>\n Ar\/\n 39<\/jats:sup>\n Ar dating experiments provided a magmatic crystallization age of 178.7\u00b12.6 Ma, and further evidence of greenschist facies crystallization during hydrothermal alteration until\n c<\/jats:italic>\n . 155 Ma. Thus, top-to-the-south obduction likely initiated along the margin of the back-arc domain, directly south of the Vedi oceanic crust, and was transported as a whole on the SAB in the Coniacian times (88\u201387 Ma). Final closure of the basin is Late Cretaceous in age (73\u201371 Ma) as dated by metamorphic rocks.\n <\/jats:p>","DOI":"10.1144\/sp340.15","type":"journal-article","created":{"date-parts":[[2010,9,14]],"date-time":"2010-09-14T18:17:53Z","timestamp":1284488273000},"page":"353-382","source":"Crossref","is-referenced-by-count":54,"title":["The Armenian Ophiolite: insights for Jurassic back-arc formation, Lower Cretaceous hot spot magmatism and Upper Cretaceous obduction over the South Armenian Block"],"prefix":"10.1144","volume":"340","author":[{"given":"Y.","family":"Rolland","sequence":"first","affiliation":[{"name":"Universit\u00e9 de Nice-Sophia Antipolis, OCA, UMR G\u00e9oAzur, CNRS, Parc Valrose, 06108 Nice cedex 2, France"}]},{"given":"G.","family":"Galoyan","sequence":"additional","affiliation":[{"name":"Universit\u00e9 de Nice-Sophia Antipolis, OCA, UMR G\u00e9oAzur, CNRS, Parc Valrose, 06108 Nice cedex 2, France"},{"name":"Institute of Geological Sciences, National Academy of Sciences of Armenia, 24a Baghramian avenue, Yerevan, 375019, Armenia"}]},{"given":"M.","family":"Sosson","sequence":"additional","affiliation":[{"name":"Universit\u00e9 de Nice-Sophia Antipolis, OCA, UMR G\u00e9oAzur, CNRS, Parc Valrose, 06108 Nice cedex 2, France"}]},{"given":"R.","family":"Melkonyan","sequence":"additional","affiliation":[{"name":"Institute of Geological Sciences, National Academy of Sciences of Armenia, 24a Baghramian avenue, Yerevan, 375019, Armenia"}]},{"given":"A.","family":"Avagyan","sequence":"additional","affiliation":[{"name":"Institute of Geological Sciences, National Academy of Sciences of Armenia, 24a Baghramian avenue, Yerevan, 375019, Armenia"}]}],"member":"1881","published-online":{"date-parts":[[2010,9,3]]},"reference":[{"key":"e_1_3_2_2_1","unstructured":"Abovyan S. 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