Výsledky vyhledávání - "Pandolfi L.[3"

LATE CRETACEOUS ARC MAGMATISM IN THE SOUTHERN CENTRAL PONTIDES: CONSTRAINTS FOR THE CLOSURE OF THE NORTHERN NEOTETHYAN BRANCHES

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

Publikováno v: Ofioliti (Bologna) 47 (2022): 19–35. doi:10.4454/ofioliti.v47i1.549
info:cnr-pdr/source/autori:Sayit K.[1], Göncüoglu M.C.[1], Ellero A.[2], Ottria G.[2], Frassi C.[3], Marroni M.[3,2], Pandolfi L.[3,2]/titolo:LATE CRETACEOUS ARC MAGMATISM IN THE SOUTHERN CENTRAL PONTIDES: CONSTRAINTS FOR THE CLOSURE OF THE NORTHERN NEOTETHYAN BRANCHES/doi:10.4454%2Fofioliti.v47i1.549/rivista:Ofioliti (Bologna)/anno:2022/pagina_da:19/pagina_a:35/intervallo_pagine:19–35/volume:47

In the southern Central Pontides in northern Turkey the remnants of two Neotethyan oceanic basins, currently represented by the Intra-Pontide and the Izmir-Ankara-Erzincan sutures, and the interposing continental microplate (i.e., the Sakarya Composi

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::73cad2060b1320291cdc295ba86da303
http://www.cnr.it/prodotto/i/463615

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Geochemistry of basaltic blueschists from the Deyader Metamorphic Complex (Makran Accretionary Prism, SE Iran): New constraints for magma generation in the Makran sector of the Neo-Tethys

Autor: Saccani E.[1], Delavari M.[2], Dolati A.[2], Pandolfi L.[3, Barbero E.[1], Tassinari R.[1], Marroni M.[3

Publikováno v: Journal of Asian earth sciences 228 (2022). doi:10.1016/j.jseaes.2022.105141
info:cnr-pdr/source/autori:Saccani E.[1], Delavari M.[2], Dolati A.[2], Pandolfi L.[3,4], Barbero E.[1], Tassinari R.[1], Marroni M.[3,4]/titolo:Geochemistry of basaltic blueschists from the Deyader Metamorphic Complex (Makran Accretionary Prism, SE Iran): New constraints for magma generation in the Makran sector of the Neo-Tethys/doi:10.1016%2Fj.jseaes.2022.105141/rivista:Journal of Asian earth sciences/anno:2022/pagina_da:/pagina_a:/intervallo_pagine:/volume:228

The North Makran Domain in the Makran Accretionary Prism consists of an imbricate stack of Mesozoic Neo Tethyan ophiolitic and metaophiolitic units. The Deyader Complex is an important metamorphic unit of this Domain and includes tectonic slices of H

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3184f23ae8855bb8dd892e66dc759931
https://publications.cnr.it/doc/466664

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The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran)

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

Publikováno v: Journal of Asian earth sciences 195 (2020): 1–26. doi:10.1016/j.jseaes.2020.104306
info:cnr-pdr/source/autori:Barbero E.[1], Delavari M.[2], Dolati A.[2], Saccani E.[1], Marroni M.[3,4], Catanzariti R.[4], Pandolfi L.[3,4]/titolo:The Ganj Complex reinterpreted as a Late Cretaceous volcanic arc: Implications for the geodynamic evolution of the North Makran domain (southeast Iran)/doi:10.1016%2Fj.jseaes.2020.104306/rivista:Journal of Asian earth sciences/anno:2020/pagina_da:1/pagina_a:26/intervallo_pagine:1–26/volume:195

The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and oceanic tectonic units. Among these, the Ganj Complex was up to now regarded as an ophiolite unit. This Complex is

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::2df655d0b9c068201b522be031ba05cf
https://doi.org/10.1016/j.jseaes.2020.104306

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Geological and geochemical evidence for a Late Cretaceous continental arc in the central Pontides, northern Turkey

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

Publikováno v: Ofioliti (Bologna) 40 (2015): 73–90. doi:10.4454/ofioliti.v40i2.436
info:cnr-pdr/source/autori:Ellero A.[1], Ottria G.[1], Sayit K.[2], Catanzariti R.[1], Frassi C.[3], Göncüoglu M.C.[2], Marroni M.[3,1], Pandolfi L.[3,1]/titolo:Geological and geochemical evidence for a Late Cretaceous continental arc in the central Pontides, northern Turkey./doi:10.4454%2Fofioliti.v40i2.436/rivista:Ofioliti (Bologna)/anno:2015/pagina_da:73/pagina_a:90/intervallo_pagine:73–90/volume:40

In the Central Pontides (Northern Turkey), south of Tosya, a tectonic unit consisting of not-metamorphic volcanic rocks and overlying sedimentary succession is exposed inside a fault-bounded elongated block. It is restrained within a wide shear zone,

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::e6ac05b616092bc053c2a45d661dc3a3

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The Jurassic association of Backarc basin ophiolites and calc-alkaline volcanics in the Guevgueli complex (northern Greece): Implication for the evolution of the Vardar zone

Autor: Saccani E.[1], Bortolotti V.[2], Marroni M.[3, Pandolfi L.[3, Photiades A.[5], Principi G.[2

Publikováno v: Ofioliti (Bologna) 33 (2008): 209–227.
info:cnr-pdr/source/autori:Saccani E.[1], Bortolotti V.[2], Marroni M.[3,4], Pandolfi L.[3,4], Photiades A.[5], Principi G.[2,4]/titolo:The Jurassic association of Backarc basin ophiolites and calc-alkaline volcanics in the Guevgueli complex (northern Greece): Implication for the evolution of the Vardar zone/doi:/rivista:Ofioliti (Bologna)/anno:2008/pagina_da:209/pagina_a:227/intervallo_pagine:209–227/volume:33

The Middle-Late Jurassic Guevgueli Complex (Greek Macedonia) represents one of the main ophiolitic complexes of the Vardar Zone and has been subdivided into two distinct sub-units, that are the East and West Guevgueli, both including intrusive and vo

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::aeef7f7b0f70ebe6aa418d3c1dbf0a40
http://www.cnr.it/prodotto/i/456642

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Geodynamic evolution of the ophiolites from Albania and Greece, (Dinaric-Hellenic belt): one, two or more oceanic basins?

Autor: Valerio Bortolotti, Gianfranco Principi, Michele Marroni, Marco Chiari, Luca Pandolfi, Emilio Saccani

Publikováno v: International journal of earth sciences (1999, Internet) 102 (2013): 783–811.
info:cnr-pdr/source/autori:Bortolotti V. [1]; Chiari M. [2]; Marroni M. [3, 4]; Pandolfi L. [3, 4]; Principi G. [1]; Saccani E. [5]/titolo:Geodynamic evolution of the ophiolites from Albania and Greece, (Dinaric-Hellenic belt): one, two or more oceanic basins?/doi:/rivista:International journal of earth sciences (1999, Internet)/anno:2013/pagina_da:783/pagina_a:811/intervallo_pagine:783–811/volume:102

All the geological constraints for an exhaustive reconstruction of the Triassic to Tertiary tectonic history of the southern Dinaric-Hellenic belt can be found in Albania and Greece. This article aims to schematically reconstruct this long tectonic e

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e7cdb88cda1bbc4f226efd2940463e43
https://publications.cnr.it/doc/209608

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