New geological, geochronological and geochemical investigations on the Khoy ophiolites and related formations, NW Iran
文摘
This paper gives a detailed geological description of the region of Khoy (NW Iran) and its ophiolites, and presents a new geological map. The main conclusion is that there are not one, but two ophiolitic complexes in the Khoy area: (1) an old, poly-metamorphic ophiolite, tectonically included within a metamorphic subduction complex, whose oldest metamorphic amphiboles yield a Lower Jurassic apparent 40Kn–40Ar age, and whose primary magmatic age should logically be pre-Jurassic; (2) a younger non metamorphic ophiolite of Upper Cretaceous age, overlain by a turbiditic, flysch-like volcanogenic series, of Upper Cretaceous-Lower Paleocene age. This latter ophiolite was created at a slow-spreading oceanic center, according to the lherzolitic mantle sequence, the small volume of gabbroic rocks, the absence of a diabasic sheeted-dike complex, and the abundant phyric basalts in the extrusive sequence. A scenario for the geodynamic evolution of the Khoy oceanic basin is proposed in conclusion.