The Bajgan Complex revealed as a Cretaceous ophiolite-bearing subduction complex: A key to unravel the geodynamics of Makran (southeast Iran)

Autor: Pandolfi L.[1, Barbero E.[3], Marroni M.[1, Delavari M.[4], Dolati A.[4], Di Rosa M.[1], Frassi C.[1], Langone A.[5], Farina F.[6], MacDonald C.S.[7], Saccani E.[3]

Publikováno v: Journal of Asian earth sciences 222 (2021): 1–23. doi:10.1016/j.jseaes.2021.104965
info:cnr-pdr/source/autori:Pandolfi L.[1,2], Barbero E.[3], Marroni M.[1,2], Delavari M.[4], Dolati A.[4], Di Rosa M.[1], Frassi C.[1], Langone A.[5], Farina F.[6], MacDonald C.S.[7], Saccani E.[3]/titolo:The Bajgan Complex revealed as a Cretaceous ophiolite-bearing subduction complex: A key to unravel the geodynamics of Makran (southeast Iran)/doi:10.1016%2Fj.jseaes.2021.104965/rivista:Journal of Asian earth sciences/anno:2021/pagina_da:1/pagina_a:23/intervallo_pagine:1–23/volume:222

In the Makran area, a wide accretionary wedge is originated by the north-dipping subduction of the Neo-Tethyan oceanic lithosphere. The rear of the accretionary wedge is represented by the North Makran Domain that consists of an imbricate stack of te

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::065a5d5e97f0596cc8427898b6531a84
http://www.cnr.it/prodotto/i/460064