Výsledky vyhledávání - "Frassi C.[1]"

The Intra-Pontide ophiolites in Northern Turkey revisited: From birth to death of a Neotethyan oceanic domain

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

Publikováno v: Geosciences Frontiers 11 (2020): 129–149. doi:10.1016/j.gsf.2019.05.010
info:cnr-pdr/source/autori:Marroni M.[1,2], Goncüoglu M.C.[3], Frassi C.[1], Sayit K.[3], Pandolfi L.[1,2], Ellero A.[2], Ottria G.[2]/titolo:The Intra-Pontide ophiolites in Northern Turkey revisited: From birth to death of a Neotethyan oceanic domain/doi:10.1016%2Fj.gsf.2019.05.010/rivista:Geosciences Frontiers/anno:2020/pagina_da:129/pagina_a:149/intervallo_pagine:129–149/volume:11
Geoscience Frontiers, Vol 11, Iss 1, Pp 129-149 (2020)

The Anatolian peninsula is a key location to study the central portion of the Neotethys Ocean(s) and to understand how its western and eastern branches were connected. One of the lesser known branches of the Mesozoic ocean(s) is preserved in the nort

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e707f3a3d0d8a9780b02aafbc83234ca
https://doi.org/10.1016/j.gsf.2019.05.010

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The Bajgan Complex revealed as a Cretaceous ophiolite-bearing subduction complex: A key to unravel the geodynamics of Makran (southeast Iran)

Autor: Pandolfi L.[1, Barbero E.[3], Marroni M.[1, Delavari M.[4], Dolati A.[4], Di Rosa M.[1], Frassi C.[1], Langone A.[5], Farina F.[6], MacDonald C.S.[7], Saccani E.[3]

Publikováno v: Journal of Asian earth sciences 222 (2021): 1–23. doi:10.1016/j.jseaes.2021.104965
info:cnr-pdr/source/autori:Pandolfi L.[1,2], Barbero E.[3], Marroni M.[1,2], Delavari M.[4], Dolati A.[4], Di Rosa M.[1], Frassi C.[1], Langone A.[5], Farina F.[6], MacDonald C.S.[7], Saccani E.[3]/titolo:The Bajgan Complex revealed as a Cretaceous ophiolite-bearing subduction complex: A key to unravel the geodynamics of Makran (southeast Iran)/doi:10.1016%2Fj.jseaes.2021.104965/rivista:Journal of Asian earth sciences/anno:2021/pagina_da:1/pagina_a:23/intervallo_pagine:1–23/volume:222

In the Makran area, a wide accretionary wedge is originated by the north-dipping subduction of the Neo-Tethyan oceanic lithosphere. The rear of the accretionary wedge is represented by the North Makran Domain that consists of an imbricate stack of te

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::065a5d5e97f0596cc8427898b6531a84
http://www.cnr.it/prodotto/i/460064

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The coupling of high-pressure oceanic and continental units in Alpine Corsica: Evidence for syn-exhumation tectonic erosion at the roof of the plate interface

Autor: Di Rosa M.[1, Meneghini F.[1], Marroni M.[1, Frassi C.[1], Pandolfi L.[1

Publikováno v: Lithos (Oslo. Print) 354-355 (2020): 1–22. doi:10.1016/j.lithos.2019.105328
info:cnr-pdr/source/autori:Di Rosa M.[1,2], Meneghini F.[1], Marroni M.[1,3], Frassi C.[1], Pandolfi L.[1,3]/titolo:The coupling of high-pressure oceanic and continental units in Alpine Corsica: Evidence for syn-exhumation tectonic erosion at the roof of the plate interface/doi:10.1016%2Fj.lithos.2019.105328/rivista:Lithos (Oslo. Print)/anno:2020/pagina_da:1/pagina_a:22/intervallo_pagine:1–22/volume:354-355

The subduction of continental crust is now a matter of fact but which are the mechanisms and the factors controlling the exhumation of continental units and their coupling with oceanic units are still a matter of debate. We herein present the tectono

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::1f3b5254651d1139605c0ea40f6a4800
https://www.journals.elsevier.com/lithos

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SYN-EXHUMATION COUPLING OF OCEANIC AND CONTINENTAL UNITS ALONG THE WESTERN EDGE OF THE ALPINE CORSICA: A REVIEW

Autor: Di Rosa M.[1], Frassi C.[1], Malasoma A.[2], Marroni M.[1, Meneghini F.[1], Pandolfi L.[1

Publikováno v: Ofioliti (Bologna) 45 (2020): 71–102. doi:10.4454/ofioliti.v45i2.533
info:cnr-pdr/source/autori:Di Rosa M.[1], Frassi C.[1], Malasoma A.[2], Marroni M.[1,3], Meneghini F.[1], Pandolfi L.[1,3]/titolo:SYN-EXHUMATION COUPLING OF OCEANIC AND CONTINENTAL UNITS ALONG THE WESTERN EDGE OF THE ALPINE CORSICA: A REVIEW/doi:10.4454%2Fofioliti.v45i2.533/rivista:Ofioliti (Bologna)/anno:2020/pagina_da:71/pagina_a:102/intervallo_pagine:71–102/volume:45

The Alpine Corsica represents a segment of the Alpine collisional belt. In its western edge, it is characterized by the close association of continental units deformed under high-pressure metamorphic conditions (Lower Units) and oceanic units showing

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::4204b60543b40610e4944bfe6333d67e
http://www.cnr.it/prodotto/i/430896

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Tectono-metamorphic evolution of the European continental margin involved in the Alpine subduction: New insights from Alpine Corsica, France

Autor: Di Rosa M.[1, Frassi C.[1], Meneghini F.[1], Marroni M.[1, Pandolfi L.[1, De Giorgi A.[1]

Publikováno v: Comptes rendus. Géoscience 351 (2019): 384–394. doi:10.1016/j.crte.2018.12.002
info:cnr-pdr/source/autori:Di Rosa M.[1,2], Frassi C.[1], Meneghini F.[1], Marroni M.[1,3], Pandolfi L.[1,3], De Giorgi A.[1]/titolo:Tectono-metamorphic evolution of the European continental margin involved in the Alpine subduction: New insights from Alpine Corsica, France/doi:10.1016%2Fj.crte.2018.12.002/rivista:Comptes rendus. Géoscience/anno:2019/pagina_da:384/pagina_a:394/intervallo_pagine:384–394/volume:351

In Corsica, continental units (the Lower Units) affected by high-pressure metamorphism represent the remains of the European margin deformed during the Alpine orogeny. In order to document how Alpine deformation and metamorphism changed along the Eur

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d2f31b278d16f52dffaffd202c66bcf5
http://hdl.handle.net/11568/1000415

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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

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Late Jurassic amphibolite-facies metamorphism in the Intra-Pontide Suture Zone (Turkey): an eastward extension of the Vardar Ocean from the Balkans

Autor: Marroni M.[1, 2] Frassi C.[1], Goncuoglu M.C., 3, Di Vincenzo G. [2], Pandolfi L.[1, Rebay G.[4] Ellero A.[2], Ottria G.[2]

Publikováno v: Journal of the Geological Society (Lond.) 171 (2014): 605–608. doi:10.1144/jgs2013-104
info:cnr-pdr/source/autori:Marroni M.[1,2] Frassi C.[1], Goncuoglu M.C.,[3], Di Vincenzo G. [2], Pandolfi L.[1,2], Rebay G.[4] Ellero A.[2], Ottria G.[2]/titolo:Late Jurassic amphibolite-facies metamorphism in the Intra-Pontide Suture Zone (Turkey): an eastward extension of the Vardar Ocean from the Balkans.../doi:10.1144%2Fjgs2013-104/rivista:Journal of the Geological Society (Lond.)/anno:2014/pagina_da:605/pagina_a:608/intervallo_pagine:605–608/volume:171

The palaeogeography of Neotethys during its closure is still a matter of debate. This study provides new insights into the Neotethys closure by the discovery in the Intra-Pontide Suture Zone (Turkey) of an accretionary complex that recorded a Late Ju

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a4ad5591a686f6612cdc10fafafaa5ad

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Geochronological constraints on post-collisional shear zones in the Variscides of Sardinia (Italy)

Autor: Carosi R. [1], Montomoli C. [1], Tiepolo M. [2], Frassi C. [1]

Publikováno v: Terra nova (Online) 24 (2012): 42–51.
info:cnr-pdr/source/autori:Carosi R. [1]; Montomoli C. [1]; Tiepolo M. [2]; Frassi C. [1]/titolo:Geochronological constraints on post-collisional shear zones in the Variscides of Sardinia (Italy)./doi:/rivista:Terra nova (Online)/anno:2012/pagina_da:42/pagina_a:51/intervallo_pagine:42–51/volume:24

The post-collisional tectonics in the inner zone of the Variscan belt of CorsicaSardinia recorded a dextral transpression developed with an orogen-parallel tectonic transport. Recent works documented the presence of nearly parallel dextral and sinist

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=cnr_________::3544b0f02e0171bc51a1acd6e150b11a
Wiley Online Library

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