THE AYLI DAG OPHIOLITE SEQUENCE (CENTRAL-NORTHERN TURKEY): A FRAGMENT OF MIDDLE JURASSIC OCEANIC LITHOSPHERE WITHIN THE INTRA-PONTIDE SUTURE ZONE

Autor: Göncüoglu M.C.[1], Marroni M.[2, Sayit K.[3], U. Kagan Tekin U.K.[5], Ottria G.[4], Pandolfi L.[2, Ellero A.[4]

Publikováno v: Ofioliti (Bologna) 37 (2012): 77–92. doi:10.4454/ofioliti.v37i2.407
info:cnr-pdr/source/autori:Göncüoglu M.C.[1], Marroni M.[2,4], Sayit K.[3], U. Kagan Tekin U.K.[5], Ottria G.[4], Pandolfi L.[2,4], Ellero A.[4]/titolo:THE AYLI DAG OPHIOLITE SEQUENCE (CENTRAL-NORTHERN TURKEY): A FRAGMENT OF MIDDLE JURASSIC OCEANIC LITHOSPHERE WITHIN THE INTRA-PONTIDE SUTURE ZONE/doi:10.4454%2Fofioliti.v37i2.407/rivista:Ofioliti (Bologna)/anno:2012/pagina_da:77/pagina_a:92/intervallo_pagine:77–92/volume:37

The Ayli Dag ophiolites occur as an independent tectonic unit within the Intra-Pontide suture zone, central-northern Turkey. They crop out, together with the other units of the Intra-Pontide suture zone, at the top of the Late Cretaceous-Middle Paleo

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http://www.cnr.it/prodotto/i/302606