The Sabzevar blueschists of the North-Central Iranian micro-continent as remnants of the Neotethys-related oceanic crust subduction

• Published in: International journal of earth sciences : Geologische Rundschau 2013-07, Vol.102 (5), p.1491-1512
• Main Authors: Omrani, Hadi, Moazzen, Mohssen, Oberhänsli, Roland, Altenberger, Uwe, Lange, Manuela
• Format: Article
• Language: English
• Subjects: Calcite; Cretaceous; Earth and Environmental Science; Earth Sciences; Eocene; Geochemistry; Geological time; Geology; Geophysics/Geodesy; Metamorphic rocks; Metamorphism; Mineral Resources; Oceanic crust; Original Paper; Petrology; Plate tectonics; Pyrite; Quartz; Sedimentology; Structural Geology
• ISSN: 1437-3254; 1437-3262
• DOI: 10.1007/s00531-013-0881-9

The Sabzevar ophiolites mark the Neotethys suture in east-north-central Iran. The Sabzevar metamorphic rocks, as part of the Cretaceous Sabzevar ophiolitic complex, consist of blueschist, amphibolite and greenschist. The Sabzevar blueschists contain sodic amphibole, epidote, phengite, calcite ± omphacite ± quartz. The epidote amphibolite is composed of sodic-calcic amphibole, epidote, albite, phengite, quartz ± omphacite, ilmenite and titanite. The greenschist contains chlorite, plagioclase and pyrite, as main minerals. Thermobarometry of a blueschist yields a pressure of 13–15.5 kbar at temperatures of 420–500 °C. Peak metamorphic temperature/depth ratios were low (~12 °C/km), consistent with metamorphism in a subduction zone. The presence of epidote in the blueschist shows that the rocks were metamorphosed entirely within the epidote stability field. Amphibole schist samples experienced pressures of 5–7 kbar and temperatures between 450 and 550 °C. The presence of chlorite, actinolite, biotite and titanite indicate greenschist facies metamorphism. Chlorite, albite and biotite replacing garnet or glaucophane suggests temperatures of >300 °C for greenschist facies. The formation of high-pressure metamorphic rocks is related to north-east-dipping subduction of the Neotethys oceanic crust and subsequent closure during lower Eocene between the Central Iranian Micro-continent and Eurasia (North Iran).