New evidence for Late Cretaceous plume-related seamounts in the Middle East sector of the Neo-Tethys: Constraints from geochemistry, petrology, and mineral chemistry of the magmatic rocks from the western Durkan Complex (Makran Accretionary Prism, SE Iran)

Autor: Barbero E.[1], Zaccarini F.[2], Delavari M.[3 ], Dolati A.[3], Saccani E.[1], Marroni M.[4, Pandolfi L.[4

Publikováno v: Lithos (Oslo. Print) 396-397 (2021): 1–22. doi:10.1016/j.lithos.2021.106228
info:cnr-pdr/source/autori:Barbero E.[1], Zaccarini F.[2], Delavari M.[3 ], Dolati A.[3], Saccani E.[1], Marroni M.[4,5], Pandolfi L.[4,5]/titolo:New evidence for Late Cretaceous plume-related seamounts in the Middle East sector of the Neo-Tethys: Constraints from geochemistry, petrology, and mineral chemistry of the magmatic rocks from the western Durkan Complex (Makran Accretionary Prism, SE Iran)/doi:10.1016%2Fj.lithos.2021.106228/rivista:Lithos (Oslo. Print)/anno:2021/pagina_da:1/pagina_a:22/intervallo_pagine:1–22/volume:396-397

The Durkan Complex in the Makran Accretionary Prism (SE Iran) has been interpreted either as a continental margin succession or a Late Cretaceous tectonically disrupted seamount chain. New whole rock and clinopyroxene chemical data for basaltic and m

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d417c006861b51c66be18307205cb47a
https://doi.org/10.1016/j.lithos.2021.106228