Fingerprinting and relocating tectonic slices along the plate interface: Evidence from the Lago Superiore unit at Monviso (Western Alps)

Autor: Gilio M.[1, Scambelluri M.[1], Agostini S.[3], Godard M.[4], Pettke T.[5], Agard P.[6], Locatelli M.[6], Angiboust S.[7]

Publikováno v: Lithos
Lithos, Elsevier, 2020, 352-353, pp.105308. ⟨10.1016/j.lithos.2019.105308⟩
Lithos (Oslo. Print) 352-353 (2020). doi:10.1016/j.lithos.2019.105308
info:cnr-pdr/source/autori:Gilio M.[1,2], Scambelluri M.[1], Agostini S.[3], Godard M.[4], Pettke T.[5], Agard P.[6], Locatelli M.[6], Angiboust S.[7]/titolo:Fingerprinting and relocating tectonic slices along the plate interface: Evidence from the Lago Superiore unit at Monviso (Western Alps)/doi:10.1016%2Fj.lithos.2019.105308/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:352-353

International audience; The Lago Superiore Unit (LSU, Monviso Massif, Italian Western Alps) is a section of fossil oceanic lithosphere equilibrated to eclogite facies conditions (550 °C – 2.8 GPa) during Alpine subduction (45–40 Ma). It is cut b

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a43c5b9bcda29c70fbe58e10967a3c8f
https://hal.umontpellier.fr/hal-02510337