Ophlolitic exposures from the East and Northeast of Nehbandan, Eastern Iran, are remnnants of a Cretaceous oceanic basin between Lut and Afghan continental blocks.They contain harzburgites, clinopyroxene-harzburgites and lherzolites equilibrated in spinel-peridotite facies. Geodynamically, the mantle tectonites record both mid-ocean ridge and supra-subduction zone signature.
Geochemistry and Petrogenesis of Mantle Peridotites from the Nehbandan Ophiolitic Complex, Eastern Iran. Journal of Applied Sciences Research, 9: 2671-2687.
SACCANI, Emilio;BECCALUVA, Luigi
2009
Abstract
Ophlolitic exposures from the East and Northeast of Nehbandan, Eastern Iran, are remnnants of a Cretaceous oceanic basin between Lut and Afghan continental blocks.They contain harzburgites, clinopyroxene-harzburgites and lherzolites equilibrated in spinel-peridotite facies. Geodynamically, the mantle tectonites record both mid-ocean ridge and supra-subduction zone signature.File in questo prodotto:
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