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Publikováno v:
Regional Geology and Tectonics: Phanerozoic Passive Margins, Cratonic Basins and Global Tectonic Maps, pp. 472–485. Amsterdam: Elsevier BV, 2012
info:cnr-pdr/source/autori:Scrocca D. (a), Carminati E.(a,b), +, Doglioni C.(a,b), Procaccianti D.(c)/titolo:Tyrrhenian Sea/titolo_volume:Regional Geology and Tectonics: Phanerozoic Passive Margins, Cratonic Basins and Global Tectonic Maps/curatori_volume:/editore: /anno:2012
info:cnr-pdr/source/autori:Scrocca D. (a), Carminati E.(a,b), +, Doglioni C.(a,b), Procaccianti D.(c)/titolo:Tyrrhenian Sea/titolo_volume:Regional Geology and Tectonics: Phanerozoic Passive Margins, Cratonic Basins and Global Tectonic Maps/curatori_volume:/editore: /anno:2012
The Tyrrhenian Sea is the easternmost basin of the western Mediterranean boudinated backarc lithosphere (where the Provençal, Valencia, and Algerian troughs also developed) in the hanging wall of the Late Oligocene to Present Apennines-Maghrebides s
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::f2b51335fc09520995fe9297e88814c1
https://doi.org/10.1016/b978-0-444-56357-6.00012-3
https://doi.org/10.1016/b978-0-444-56357-6.00012-3
