Zobrazeno 1 - 5
of 5
pro vyhledávání: '"Ellero A.[2]"'
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)
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
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
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
http://www.cnr.it/prodotto/i/463615
Autor:
Goncuoglu M.C.[1], Marroni M. [1, Pandolfi L.[2, Ellero A.[2], Ottria G. [2], Catanzariti R.[2], Tekin U. K.[4], Sayit K. [1
Publikováno v:
Journal of Asian earth sciences 85 (2014): 117–139. doi:10.1016/j.jseaes.2014.01.013
info:cnr-pdr/source/autori:Goncuoglu M.C.[1], Marroni M. [1,2], Pandolfi L.[2,3], Ellero A.[2], Ottria G. [2], Catanzariti R.[2], Tekin U. K.[4], Sayit K. [1,5]/titolo:The Arkot Dag Melange in Arac area, central Turkey: Evidence of its origin within the geodynamic evolution of the Intra-Pontide suture zone/doi:10.1016%2Fj.jseaes.2014.01.013/rivista:Journal of Asian earth sciences/anno:2014/pagina_da:117/pagina_a:139/intervallo_pagine:117–139/volume:85
info:cnr-pdr/source/autori:Goncuoglu M.C.[1], Marroni M. [1,2], Pandolfi L.[2,3], Ellero A.[2], Ottria G. [2], Catanzariti R.[2], Tekin U. K.[4], Sayit K. [1,5]/titolo:The Arkot Dag Melange in Arac area, central Turkey: Evidence of its origin within the geodynamic evolution of the Intra-Pontide suture zone/doi:10.1016%2Fj.jseaes.2014.01.013/rivista:Journal of Asian earth sciences/anno:2014/pagina_da:117/pagina_a:139/intervallo_pagine:117–139/volume:85
In northern Turkey, the Intra-Pontide suture zone is represented by an east–west trending belt of deformed and/or metamorphic units located at the boundary between the Istanbul–Zonguldak terrane to the north and the Sakarya terrane to the south.
Autor:
Barazzuoli P.[1], Bertini G.[2], Brogi A.[3], Capezzuoli E.[4], Conticelli S.[5], Doveri M.[2], Ellero A.[2], Gianelli G. [2], La Felice S.[2], Liotta D.[3, Marroni M.[6], Manzella A.[2], Meccheri M.[1], Montanari D.[7], Pandeli E.[5], Principe C.[2], Ruggieri G.[2], Sbrana A.[6], Vaselli O.[5, Vezzoli L.[8
Publikováno v:
Journal of volcanology and geothermal research 303 (2015): 1–6. doi:10.1016/j.jvolgeores.2015.07.004
info:cnr-pdr/source/autori:Barazzuoli P.[1], Bertini G.[2], Brogi A.[3], Capezzuoli E.[4], Conticelli S.[5], Doveri M.[2], Ellero A.[2], Gianelli G. [2], La Felice S.[2], Liotta D.[3,2], Marroni M.[6], Manzella A.[2], Meccheri M.[1], Montanari D.[7], Pandeli E.[5], Principe C.[2], Ruggieri G.[2], Sbrana A.[6], Vaselli O.[5,2], Vezzoli L.[8,2]/titolo:Comment on: "Borgia A., Mazzoldi A., Brunori C.A., Allocca C., Delcroix C., Micheli L., Vercellino A., Grieco, G., 2014. Volcanic spreading forcing and feedback in geothermal reservoir development,Amiata Volcano,Italia. J. Volc. Geoth. Res. 284, 16-31/doi:10.1016%2Fj.jvolgeores.2015.07.004/rivista:Journal of volcanology and geothermal research/anno:2015/pagina_da:1/pagina_a:6/intervallo_pagine:1–6/volume:303
info:cnr-pdr/source/autori:Barazzuoli P.[1], Bertini G.[2], Brogi A.[3], Capezzuoli E.[4], Conticelli S.[5], Doveri M.[2], Ellero A.[2], Gianelli G. [2], La Felice S.[2], Liotta D.[3,2], Marroni M.[6], Manzella A.[2], Meccheri M.[1], Montanari D.[7], Pandeli E.[5], Principe C.[2], Ruggieri G.[2], Sbrana A.[6], Vaselli O.[5,2], Vezzoli L.[8,2]/titolo:Comment on: "Borgia A., Mazzoldi A., Brunori C.A., Allocca C., Delcroix C., Micheli L., Vercellino A., Grieco, G., 2014. Volcanic spreading forcing and feedback in geothermal reservoir development,Amiata Volcano,Italia. J. Volc. Geoth. Res. 284, 16-31/doi:10.1016%2Fj.jvolgeores.2015.07.004/rivista:Journal of volcanology and geothermal research/anno:2015/pagina_da:1/pagina_a:6/intervallo_pagine:1–6/volume:303
Borgia et al. (2014) illustrated an active volcanic spreading model for the Amiata volcanic area (southern Tuscany, Italy). Although, at first glance, the model may appear appealing, this is not fully supported by the available data and the paper doe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::1bc188ba886150402e588db9e4ee9626
https://publications.cnr.it/doc/334303
https://publications.cnr.it/doc/334303
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
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