Zobrazeno 1 - 6
of 6
pro vyhledávání: '"AGOSTINI S.[1]"'
Publikováno v:
Scientific Reports
Scientific reports (Nature Publishing Group) 11 (2021): 1–13. doi:10.1038/s41598-021-90275-7
info:cnr-pdr/source/autori:Agostini S.[1], Di Giuseppe P.[1], Manetti P.[2], Doglioni C.[3,4], Conticelli S.[2,5]/titolo:A heterogeneous subcontinental mantle under the African-Arabian Plate boundary revealed by boron and radiogenic isotopes/doi:10.1038%2Fs41598-021-90275-7/rivista:Scientific reports (Nature Publishing Group)/anno:2021/pagina_da:1/pagina_a:13/intervallo_pagine:1–13/volume:11
Scientific Reports, Vol 11, Iss 1, Pp 1-13 (2021)
Scientific reports (Nature Publishing Group) 11 (2021): 1–13. doi:10.1038/s41598-021-90275-7
info:cnr-pdr/source/autori:Agostini S.[1], Di Giuseppe P.[1], Manetti P.[2], Doglioni C.[3,4], Conticelli S.[2,5]/titolo:A heterogeneous subcontinental mantle under the African-Arabian Plate boundary revealed by boron and radiogenic isotopes/doi:10.1038%2Fs41598-021-90275-7/rivista:Scientific reports (Nature Publishing Group)/anno:2021/pagina_da:1/pagina_a:13/intervallo_pagine:1–13/volume:11
Scientific Reports, Vol 11, Iss 1, Pp 1-13 (2021)
The northern and northwestern margins of the Arabian Plate are a locus of a diffuse and long-lasting (early Miocene to Pleistocene) Na-alkali basaltic volcanism, sourced in the asthenosphere mantle. The upwelling asthenosphere at the Africa–Arabia
Publikováno v:
Earth-science reviews 221 (2021): 1–13. doi:10.1016/j.earscirev.2021.103785
info:cnr-pdr/source/autori:Cornacchia I.[1], Brandano M.[2,3], Agostini S.[1]/titolo:Miocene paleoceanographic evolution of the Mediterranean area and carbonate production changes: A review/doi:10.1016%2Fj.earscirev.2021.103785/rivista:Earth-science reviews/anno:2021/pagina_da:1/pagina_a:13/intervallo_pagine:1–13/volume:221
info:cnr-pdr/source/autori:Cornacchia I.[1], Brandano M.[2,3], Agostini S.[1]/titolo:Miocene paleoceanographic evolution of the Mediterranean area and carbonate production changes: A review/doi:10.1016%2Fj.earscirev.2021.103785/rivista:Earth-science reviews/anno:2021/pagina_da:1/pagina_a:13/intervallo_pagine:1–13/volume:221
Miocene is a key interval in the global climate evolution as well as in the geodynamic evolution of the Mediterranean basin. Therefore, global and regional factors controlled Miocene Mediterranean oceanography, which, in turn, affected carbonate prod
Autor:
Agostini S.[1], Savascin M.[2], Di Giuseppe P.[1, Di Stefano F.[4], Karaoglu O.[5], Lustrino M.[4, Manetti P.[7, Ersoy Y.[8], Kürüm S.[9], Önal A.[2]
Publikováno v:
Italian Journal of Geosciences (Online) 138 (2019): 435–455.
info:cnr-pdr/source/autori:Agostini S.[1], Savascin M.[2], Di Giuseppe P.[1,3], Di Stefano F.[4], Karaoglu O.[5], Lustrino M.[4,6], Manetti P.[7,1], Ersoy Y.[8], Kürüm S.[9], Önal A.[2]/titolo:Neogene volcanism in Elazig-Tunceli area (eastern Anatolia): geochronological and petrological constraints/doi:/rivista:Italian Journal of Geosciences (Online)/anno:2019/pagina_da:435/pagina_a:455/intervallo_pagine:435–455/volume:138
info:cnr-pdr/source/autori:Agostini S.[1], Savascin M.[2], Di Giuseppe P.[1,3], Di Stefano F.[4], Karaoglu O.[5], Lustrino M.[4,6], Manetti P.[7,1], Ersoy Y.[8], Kürüm S.[9], Önal A.[2]/titolo:Neogene volcanism in Elazig-Tunceli area (eastern Anatolia): geochronological and petrological constraints/doi:/rivista:Italian Journal of Geosciences (Online)/anno:2019/pagina_da:435/pagina_a:455/intervallo_pagine:435–455/volume:138
The Elaz?? and Tunceli provinces in eastern Anatolia host a complex succession of Miocene-Pleistocene effusive and explosive volcanic rocks, divided into four distinct volcanic phases. The most abundant and widespread products are the calcalkaline Ma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::9f9c389ae996e7fcb8467d21152e2de9
http://www.cnr.it/prodotto/i/407686
http://www.cnr.it/prodotto/i/407686
Publikováno v:
Geochemistry, geophysics, geosystems 8 (2007): 1–18. doi:10.1029/2006GC001508
info:cnr-pdr/source/autori:Tonarini S.(1); Agostini S.(1); Doglioni C.(2); Innocenti F.(3,1); Manetti P.(1)/titolo:Evidence for serpentinite fluid in convergent margin systems: the example of El Salvador (central America) arc lavas./doi:10.1029%2F2006GC001508/rivista:Geochemistry, geophysics, geosystems/anno:2007/pagina_da:1/pagina_a:18/intervallo_pagine:1–18/volume:8
info:cnr-pdr/source/autori:Tonarini S.(1); Agostini S.(1); Doglioni C.(2); Innocenti F.(3,1); Manetti P.(1)/titolo:Evidence for serpentinite fluid in convergent margin systems: the example of El Salvador (central America) arc lavas./doi:10.1029%2F2006GC001508/rivista:Geochemistry, geophysics, geosystems/anno:2007/pagina_da:1/pagina_a:18/intervallo_pagine:1–18/volume:8
A comprehensive geochemical study, including B, Pb, Sr, and Nd isotopes, has been carried out on El Salvador subduction-related lavas. The rocks have arc-type incompatible element distributions with high LILE/HFSE ratios, nearly constant 143Nd/144Nd
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::d58d70cd3eb382d4f9681b11ac39ba71
http://hdl.handle.net/11573/81023
http://hdl.handle.net/11573/81023
Publikováno v:
Coordination chemistry reviews
250 (2006): 561–573.
info:cnr-pdr/source/autori:Bandoli G. 1, Tisato F. 2, Dolmella A. 1, Agostini S. 1/titolo:Structural overview of technetium compounds (20002004)/doi:/rivista:Coordination chemistry reviews (Print)/anno:2006/pagina_da:561/pagina_a:573/intervallo_pagine:561–573/volume:250
250 (2006): 561–573.
info:cnr-pdr/source/autori:Bandoli G. 1, Tisato F. 2, Dolmella A. 1, Agostini S. 1/titolo:Structural overview of technetium compounds (20002004)/doi:/rivista:Coordination chemistry reviews (Print)/anno:2006/pagina_da:561/pagina_a:573/intervallo_pagine:561–573/volume:250
This paper provides an overview of the about 80 crystal structures of technetium complexes described in the past 5 years and exhibiting some peculiar structural features. In almost 90% of the compounds, technetium shows an odd oxidation number, and b
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::4826868a60e93075ac0c4ee44b0a4e2a
http://www.cnr.it/prodotto/i/18350
http://www.cnr.it/prodotto/i/18350
Autor:
AGOSTINI S.[1], DI VINCENZO G.[1], DOGLIONI C.[2], INNOCENTI F.[3], MANETTI P.[4], SAVASCIN M.Y.[5], TONARINI S.[1]
Publikováno v:
EGS-AGU-EUG Joint Assembly, Nice, France, 6-11 April 2003
info:cnr-pdr/source/autori:AGOSTINI S.[1], DI VINCENZO G.[1], DOGLIONI C.[2], INNOCENTI F.[3], MANETTI P.[4], SAVASCIN M.Y.[5], TONARINI S.[1]/congresso_nome:EGS-AGU-EUG Joint Assembly/congresso_luogo:Nice, France/congresso_data:6-11 April 2003/anno:2003/pagina_da:/pagina_a:/intervallo_pagine
info:cnr-pdr/source/autori:AGOSTINI S.[1], DI VINCENZO G.[1], DOGLIONI C.[2], INNOCENTI F.[3], MANETTI P.[4], SAVASCIN M.Y.[5], TONARINI S.[1]/congresso_nome:EGS-AGU-EUG Joint Assembly/congresso_luogo:Nice, France/congresso_data:6-11 April 2003/anno:2003/pagina_da:/pagina_a:/intervallo_pagine
No abstract
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=cnr_________::7194b804b35bad214e4d8bca34413077
https://publications.cnr.it/doc/111420
https://publications.cnr.it/doc/111420