Seawater-originated fluids interactions with oceanic lithospheric mantle peridotites and formation of hornblendite dykes, as well as spadaite and dolomite veins in the Naein ophiolite (Isfahan Province, Iran)

The Mesozoic ophiolitic mélange of Naein is located to the west of the Central-East Iranian Microcontinent (CEIM). In this ophiolite, the mantle peridotites cross cut by greenish, coarse-grained hornblendite dykes with up to 50 cm width. These dykes cross cut by carbonate veins with a few millimeter...

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Autores principales:	Fatemeh Naderi, Ghodrat Torabi, Nargess Shirdashtzadeh
Formato:	Artigo
Lenguaje:	Persa
Publicado:	Ferdowsi University of Mashhad 2024-12-01
Colección:	Journal of Economic Geology
Materias:	seawater-derived fluids the fluid-rock interaction hornblendite spadaite carbonate veins mantle peridotites of the naein ophiolite central east- iranian microcontinent (ceim)
Acceso en línea:	https://econg.um.ac.ir/article_45983.html?lang=en
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