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- W1572126075 abstract "The Nain-Baft ophiolitic suture, along the active margin of the Central Iranian continental block (the Sanandaj-Sirjan zone) features back-arc extension during the Late Mesozoic. This ophiolitic belt is characterized by occurrence of mafic lavas including pillow lavas, diabasic dikes and layers, massive basaltic lavas and basaltic-andesitic rock fragments in the volcanic breccias. These mafic lavas display both calc-alkaline and island-arc tholeiitic affinities with enrichment in LILE and depletion in HFSE. Conventional K-Ar measurements on amphibole indicate the Middle Cretaceous for the creation and evolution of the Nain-Baft back-arc basins. As a result of oblique subduction of the Tethyan Ocean, a narrow transtensional back-arc basin could start to open along large transcurrent faults in the active margin of the Iranian continental block." @default.
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- W1572126075 date "2008-01-07" @default.
- W1572126075 modified "2023-09-26" @default.
- W1572126075 title "MESOZOIC BACK-ARC EXTENSION IN THE ACTIVE MARGIN OF THE IRANIAN CONTINENTAL BLOCK: CONSTRAINTS FROM AGE AND GEOCHEMISTRY OF THE MAFIC LAVAS" @default.
- W1572126075 doi "https://doi.org/10.4454/ofioliti.v33i2.362" @default.
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