Subduction-related hybridization of the lithospheric mantle revealed by trace element and Sr-Nd-Pb isotopic data in composite xenoliths from Tallante (Betic Cordillera, Spain)

Autor: Avanzinelli R.[1, Bianchini G.[3], Tiepolo M.[4], Jasim A.[1, Natali C.[1], Braschi E.[2], Dallai L.[6], Beccaluva L.[3], Conticelli S.[1

Publikováno v: Lithos (Oslo. Print) 352-353 (2020): 1–17. doi:10.1016/j.lithos.2019.105316
info:cnr-pdr/source/autori:Avanzinelli R.[1,2], Bianchini G.[3], Tiepolo M.[4], Jasim A.[1,5], Natali C.[1], Braschi E.[2], Dallai L.[6], Beccaluva L.[3], Conticelli S.[1,7]/titolo:Subduction-related hybridization of the lithospheric mantle revealed by trace element and Sr-Nd-Pb isotopic data in composite xenoliths from Tallante (Betic Cordillera, Spain)/doi:10.1016%2Fj.lithos.2019.105316/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:1/pagina_a:17/intervallo_pagine:1–17/volume:352-353

Ultramafic xenoliths are rarely found at convergent plate margins. A notable exception is in the Betic Cordillera of southern Spain, where the eruption of xenolith-bearing alkaline basalts during the Pliocene post-dated the Cenozoic phase of plate co

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8dcf219ec43ec245bbe2a1aa6aea2581
http://hdl.handle.net/2158/1192267