Zobrazeno 1 - 2
of 2
pro vyhledávání: '"Jourdan F.[2]"'
Autor:
Brombin V.[1], Bonadiman C.[1], Jourdan F.[2], Roghi G.[3], Coltorti M.[1], Webb L.E.[4], Callegaro S.[5], Bellieni G.[6], De Vecchi G.[6], Sede R.[1, Marzoli A.[3
Publikováno v:
Earth-science reviews 192 (2019): 355–378. doi:10.1016/j.earscirev.2019.03.016
info:cnr-pdr/source/autori:Brombin V.[1], Bonadiman C.[1], Jourdan F.[2], Roghi G.[3], Coltorti M.[1], Webb L.E.[4], Callegaro S.[5], Bellieni G.[6], De Vecchi G.[6], Sede R.[1,6], Marzoli A.[3,6]/titolo:Intraplate magmatism at a convergent plate boundary: The case of the Cenozoic northern Adria magmatism/doi:10.1016%2Fj.earscirev.2019.03.016/rivista:Earth-science reviews/anno:2019/pagina_da:355/pagina_a:378/intervallo_pagine:355–378/volume:192
info:cnr-pdr/source/autori:Brombin V.[1], Bonadiman C.[1], Jourdan F.[2], Roghi G.[3], Coltorti M.[1], Webb L.E.[4], Callegaro S.[5], Bellieni G.[6], De Vecchi G.[6], Sede R.[1,6], Marzoli A.[3,6]/titolo:Intraplate magmatism at a convergent plate boundary: The case of the Cenozoic northern Adria magmatism/doi:10.1016%2Fj.earscirev.2019.03.016/rivista:Earth-science reviews/anno:2019/pagina_da:355/pagina_a:378/intervallo_pagine:355–378/volume:192
The complex European–Adria geodynamic framework, which led to the formation of the Alpine belt, is considered responsible for the orogenic magmatism that occurred in the Central Alps along the Periadriatic/Insubric Line (late Eocene–early Oligoce
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::a6be5f0574f40f5fff99414592a1c027
https://publications.cnr.it/doc/463572
https://publications.cnr.it/doc/463572
Publikováno v:
Lithos, Vol. 188 (2014) pp. 44-59
Lithos (Oslo. Print) 188 (2014): 44–59. doi:10.1016/j.lithos.2013.09.013
info:cnr-pdr/source/autori:Marzoli A. [1,6], Jourdan F. [2], Bussy F.[3], Chiaradia M. [4], Costa F. [4]/titolo:Petrogenesis of tholeiitic basalts from the Central Atlantic magmatic province as revealed by mineral major and trace elements and Sr isotopes./doi:10.1016%2Fj.lithos.2013.09.013/rivista:Lithos (Oslo. Print)/anno:2014/pagina_da:44/pagina_a:59/intervallo_pagine:44–59/volume:188
Lithos (Oslo. Print) 188 (2014): 44–59. doi:10.1016/j.lithos.2013.09.013
info:cnr-pdr/source/autori:Marzoli A. [1,6], Jourdan F. [2], Bussy F.[3], Chiaradia M. [4], Costa F. [4]/titolo:Petrogenesis of tholeiitic basalts from the Central Atlantic magmatic province as revealed by mineral major and trace elements and Sr isotopes./doi:10.1016%2Fj.lithos.2013.09.013/rivista:Lithos (Oslo. Print)/anno:2014/pagina_da:44/pagina_a:59/intervallo_pagine:44–59/volume:188
The petrogenesis of the Kerforne dyke tholeiitic basalts (Brittany, France), the northernmost outcrop of the 200 Ma Central Atlantic magmatic province (CAMP), is constrained by its zoned augite and plagioclase crystals. Augite cores with high Mg/Fe a
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::3161d8696290d6bb09c06018af26f717
http://hdl.handle.net/11577/2790300
http://hdl.handle.net/11577/2790300