Výsledky vyhledávání - "PANDOLFI L.(4)"

New evidence for Late Cretaceous plume-related seamounts in the Middle East sector of the Neo-Tethys: Constraints from geochemistry, petrology, and mineral chemistry of the magmatic rocks from the western Durkan Complex (Makran Accretionary Prism, SE Iran)

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

Publikováno v: Lithos (Oslo. Print) 396-397 (2021): 1–22. doi:10.1016/j.lithos.2021.106228
info:cnr-pdr/source/autori:Barbero E.[1], Zaccarini F.[2], Delavari M.[3 ], Dolati A.[3], Saccani E.[1], Marroni M.[4,5], Pandolfi L.[4,5]/titolo:New evidence for Late Cretaceous plume-related seamounts in the Middle East sector of the Neo-Tethys: Constraints from geochemistry, petrology, and mineral chemistry of the magmatic rocks from the western Durkan Complex (Makran Accretionary Prism, SE Iran)/doi:10.1016%2Fj.lithos.2021.106228/rivista:Lithos (Oslo. Print)/anno:2021/pagina_da:1/pagina_a:22/intervallo_pagine:1–22/volume:396-397

The Durkan Complex in the Makran Accretionary Prism (SE Iran) has been interpreted either as a continental margin succession or a Late Cretaceous tectonically disrupted seamount chain. New whole rock and clinopyroxene chemical data for basaltic and m

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d417c006861b51c66be18307205cb47a
https://doi.org/10.1016/j.lithos.2021.106228

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Early Cretaceous Plume–Ridge Interaction Recorded in the Band-e-Zeyarat Ophiolite (North Makran, Iran): New Constraints from Petrological, Mineral Chemistry, and Geochronological Data

Autor: Barbero E.[1], Delavari M.[2], Dolati A.[2], Vahedi L.[2], Langone A.[3], Marroni M.[4, Pandolfi L.[4, Zaccarini F.[6] Saccani E.[1]

Publikováno v: Minerals, Vol 10, Iss 1100, p 1100 (2020)
Minerals (Basel) 10 (2020): 1–36. doi:10.3390/min10121100
info:cnr-pdr/source/autori:Barbero E.[1], Delavari M.[2], Dolati A.[2], Vahedi L.[2], Langone A.[3], Marroni M.[4,5], Pandolfi L.[4,5], Zaccarini F.[6] Saccani E.[1]/titolo:Early cretaceous plume-ridge interaction recorded in the band-e-zeyarat ophiolite (North Makran, Iran): New constraints from petrological, mineral chemistry, and geochronological data/doi:10.3390%2Fmin10121100/rivista:Minerals (Basel)/anno:2020/pagina_da:1/pagina_a:36/intervallo_pagine:1–36/volume:10
Minerals
Volume 10
Issue 12

The North Makran domain (southeast Iran) is part of the Makran accretionary wedge and consists of an imbricate stack of continental and Neo-Tethyan oceanic tectonic units. Among these, the Band-e-Zeyarat ophiolite consists of (from bottom to top): ul

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4c4c0c206a25ec1a9e4aa5ae8504a94e
http://hdl.handle.net/11392/2432003

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The stratigraphic and structural setting of metamorphic continental units from Alpine Corsica: clues from the area between Asco and Golo valleys (Central Corsica, France)

Autor: Malasoma A.[1], Morelli G.[2, Di Rosa M.[4], Marroni M.[4, Pandeli E.[2, Principi G.[3], Pandolfi L.[4

Publikováno v: Journal of maps 16 (2020): 313–323. doi:10.1080/17445647.2020.1746421
info:cnr-pdr/source/autori:Malasoma A.[1], Morelli G.[2,3], Di Rosa M.[4], Marroni M.[4,5], Pandeli E.[2,3], Principi G.[3], Pandolfi L.[4,5]/titolo:The stratigraphic and structural setting of metamorphic continental units from Alpine Corsica: clues from the area between Asco and Golo valleys (Central Corsica, France)/doi:10.1080%2F17445647.2020.1746421/rivista:Journal of maps/anno:2020/pagina_da:313/pagina_a:323/intervallo_pagine:313–323/volume:16
Journal of Maps, Vol 16, Iss 2, Pp 313-323 (2020)

The area between the Asco and Golo valleys in Central Corsica, France (latitudes 42°47′95″N to 42°37′96″N, longitudes from 9°11′82″E to 9°20′72″E) is a key-sector to investigate the stratigraphic and tectonic setting of Alpine Cor

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=doi_dedup___::6ee9de3c53019622c1431b19238cfc54

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Northern Apennine and Corsican ophiolites: the oceanic lithosphere of the Ligure-Piemontese basin and its transition to the Adria continental margin (Italy)

Autor: BORTOLOTTI V. (1), CORTESOGNO L.(2), GAGGERO L.(2), LAHONDERE D.(3), MARRONI M.(4), MOLLI G.(4), M., MONTANINI E.(5), PANDOLFI L.(4), PRINCIPI G.(6), ROSSI P.(3), SACCANI E.(7), TREVES B.(1), TRIBUZIO R.(8)

Publikováno v: Memorie descrittive della carta geologica d'Italia 63 (2004): 1–52.
info:cnr-pdr/source/autori:BORTOLOTTI V. (1); CORTESOGNO L.(2); GAGGERO L.(2); LAHONDERE D.(3); MARRONI M.(4); MOLLI G.(4); M., MONTANINI E.(5); PANDOLFI L.(4); PRINCIPI G.(6); ROSSI P.(3); SACCANI E.(7); TREVES B.(1); & TRIBUZIO R.(8)/titolo:Northern Apennine and Corsica ophiolites: the oceanic lithosphere of the Ligure-Piemontese basin and its transition to the Adria continental margin (Italy)./doi:/rivista:Memorie descrittive della carta geologica d'Italia/anno:2004/pagina_da:1/pagina_a:52/intervallo_pagine:1–52/volume:63

Externí odkaz: https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::086bbfbb0f89e8ea710bb3cd81c143bf
http://hdl.handle.net/11568/90316

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