Metamorphic imprint of ridge subduction on the Neo-Tethyan ophiolites from the Saka Unit (Central Pontides, northern Turkey)

Autor: Frassi C.[1], Rebay G.[2], Marroni M.[1, Sayit K. [4], Göncüoglu M.C.[4], Ellero A.[3], Ottria G.[3], Pandolfi L.[1

Publikováno v: Journal of Asian earth sciences 200 (2020). doi:10.1016/j.jseaes.2020.104468
info:cnr-pdr/source/autori:Frassi C.[1], Rebay G.[2], Marroni M.[1,3], Sayit K. [4], Göncüoglu M.C.[4], Ellero A.[3], Ottria G.[3], Pandolfi L.[1,3]/titolo:Metamorphic imprint of ridge subduction on the Neo-Tethyan ophiolites from the Saka Unit (Central Pontides, northern Turkey)/doi:10.1016%2Fj.jseaes.2020.104468/rivista:Journal of Asian earth sciences/anno:2020/pagina_da:/pagina_a:/intervallo_pagine:/volume:200

The Intra-Pontide suture zone is the northernmost ophiolite suture zone exposed in the Anatolian peninsula. It consists of several variably deformed and metamorphosed tectonic units derived from the Neo-Tethyan Intra-Pontide oceanic (IPO) basin, and

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e6c4b34e6d9358773b89234fe4e60472
http://hdl.handle.net/11568/1064731