Zobrazeno 1 - 10
of 37
pro vyhledávání: '"Alfonso Bosellini"'
Autor:
ALFONSO BOSELLINI, FRANCESCA R. BOSELLINI, MARIA LUISA COLALONGO, MARIANO PARENTE, ANTONIO RUSSO, ALESSANDRO VESCOGNI
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 105, Iss 3 (1999)
The Cretaceous to Quaternary succession of the Apulia Platform cropping out on the eastern coast of the Salento Peninsula shows a special stratigraphic architecture. Whereas on the platform top, i.e. on the Salento Peninsula proper, the succession is
Externí odkaz:
https://doaj.org/article/1fed4af5ebb24f3a868bfdf3dba5b731
Autor:
MICHELE MORSILLI, ALFONSO BOSELLINI
Publikováno v:
Rivista Italiana di Paleontologia e Stratigrafia, Vol 103, Iss 2 (1997)
The Late Jurassic-Early Cretaceous Apulia platform margin and the transition to adjacent basinal deposits (inner platform to basin) are well exposed in the Gargano Promontory. Detailed field work has allowed to recognize eight main facies association
Externí odkaz:
https://doaj.org/article/1e02fe35d8d44f4a818a8da98e897f3f
Autor:
Alfonso Bosellini
Publikováno v:
World Geomorphological Landscapes ISBN: 9783319261928
The Italian peninsula is an extremely active region from the geodynamic point of view as witnessed by the presence of active volcanoes (Vesuvius, Campi Flegrei, Stromboli, Vulcano, Etna) and by frequent earthquakes. Italian geology, however, is domin
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eb0cac2e84aa514bf38f8926cfd15e86
https://doi.org/10.1007/978-3-319-26194-2_3
https://doi.org/10.1007/978-3-319-26194-2_3
Publikováno v:
International Journal of Earth Sciences. 91:315-330
Synthetic seismic models of outcrops in the Early Cretaceous slope of a carbonate platform on the Gargano Promontory (southern Italy) were compared to an offshore seismic section south of the Promontory. Outcrops of the same age on the promontory hav
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::89c628253ebce2308fbae4681574b8f6
https://doi.org/10.1007/s005310100213
https://doi.org/10.1007/s005310100213
Publikováno v:
Journal of African Earth Sciences. 32:403-417
The Mesozoic succession of Dire Dawa, Harar Province, Ethiopia, consists of a lower fluviatile sandstone (Adigrat Sandstone); an intermediate carbonate-marly unit, formerly called Antalo Limestone; and an upper fluviatile sandstone (Amba Aradam Forma
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::10564764c69a06ab942736722f044ad8
https://doi.org/10.1016/s0899-5362(01)90105-8
https://doi.org/10.1016/s0899-5362(01)90105-8
Publikováno v:
Cretaceous Research. 20:783-791
The occurrence of a thin band of marine limestone (Graua Limestone) within a thick succession of fluviatile sandstones in south-eastern Ethiopia is direct evidence of flooding of part of the East African craton (Horn of Africa). According to the pres
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::b03c2b32b32ef9add9cb9678c607c599
https://doi.org/10.1006/cres.1999.0183
https://doi.org/10.1006/cres.1999.0183
Publikováno v:
Rendiconti Lincei. 6:253-267
Nella sua area-tipo il Calcare di Antalo (Oxfordiano-Kimmeridgiano) risulta costituito da gruppi di cicli o parasequenze, retrogradanti nella parte inferiore, aggradanti in quella centrale e progradanti in quella superiore. Questa organizzazione stra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d67c54a5a47bc321dee88374ede039d9
https://doi.org/10.1007/bf03001687
https://doi.org/10.1007/bf03001687
Publikováno v:
Scopus-Elsevier
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::4b3bef2fad09368c859d40855ba29e32
http://hdl.handle.net/11392/1198284
http://hdl.handle.net/11392/1198284
Publikováno v:
SEPM Journal of Sedimentary Research. 69
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::6798cfcd59fb0aea811b361d9393e59c
https://doi.org/10.1306/d4268b4e-2b26-11d7-8648000102c1865d
https://doi.org/10.1306/d4268b4e-2b26-11d7-8648000102c1865d
The study of two Lower Cretaceous stratigraphic sections from northern Gargano, Apulia, southern Italy, has shown that the classic succession of the Umbria-Marche Basin, central Italy, can be extended to the south as far as the Gargano Promontory. He
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::763ed32811d791787e1741e8fc81b73c
http://hdl.handle.net/11392/1198289
http://hdl.handle.net/11392/1198289