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pro vyhledávání: '"Azzurra d'Atri"'
Eocene-Oligocene paleogeographic/paleotectonic reconstructions of the Rhodopian - northern Aegean - western Black Sea region largely ignore the Thrace Basin, a large sedimentary basin up to 9 km thick that has been long interpreted as a forearc basin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::134e065508e0f9347623149ce0b75c2e
http://hdl.handle.net/11585/531297
http://hdl.handle.net/11585/531297
Publikováno v:
Sedimentary Geology 243-244 (2012): 117–129.
info:cnr-pdr/source/autori:D'Atri A. [1]; Zuffa G. G. [1]; Cavazza W. [1]; Okay A. [2]; Di Vincenzo G. [3]/titolo:Detrital supply from subduction%2Faccretion complexes to the Eocene-Oligocene post-collisional southern Thrace Basin (NW Turkey and NE Greece)./doi:/rivista:Sedimentary Geology/anno:2012/pagina_da:117/pagina_a:129/intervallo_pagine:117–129/volume:243-244
info:cnr-pdr/source/autori:D'Atri A. [1]; Zuffa G. G. [1]; Cavazza W. [1]; Okay A. [2]; Di Vincenzo G. [3]/titolo:Detrital supply from subduction%2Faccretion complexes to the Eocene-Oligocene post-collisional southern Thrace Basin (NW Turkey and NE Greece)./doi:/rivista:Sedimentary Geology/anno:2012/pagina_da:117/pagina_a:129/intervallo_pagine:117–129/volume:243-244
The Thrace Basin is a large, mostly Eocene–Oligocene post-collisional sedimentary basin which developed following the closure of the Vardar–Izmir–Ankara oceanic domain (latest Cretaceous–Paleocene). Sandstone petrologic data (framework and he
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::e86d45d1e5d58c95fedaec452b002366
http://scienceserver.cilea.it/cgi-bin/sciserv.pl?collection=journals&journal=00370738
http://scienceserver.cilea.it/cgi-bin/sciserv.pl?collection=journals&journal=00370738