Zobrazeno 1 - 10
of 55
pro vyhledávání: '"Mauro Caffau"'
Autor:
Mauro Caffau, Mario Pleničar
Publikováno v:
Geologija, Vol 47, Iss 1, Pp 41-54 (2004)
The Santonian-Campanian limestones of Nanos Mountain are mainly characterized by wackestone-packstone with benthic foraminifers, thaumatoporellaceans and rudists. Rudists in growth position are rare and rudist congregations are found only in bouquets
Externí odkaz:
https://doaj.org/article/ba79dc12ebb742aab953229df853a5bf
Bournonia excavata (D’Orbigny) from the Campanian-Maastrichtian of Stranice (north-east of Slovenia)
Autor:
Mauro Caffau
Publikováno v:
Geologija, Vol 45, Iss 1, Pp 91-96 (2002)
The rudist fauna of Stranice, in the north-east of Slovenia, has been studied for a long time thanks to the good preservation-state of the specimens found in the calcareous breccias from Campanian-Maastrichtian. The presence of Bournonia excavata (d
Externí odkaz:
https://doaj.org/article/00c70b16dd8943eab135bbcf58d8df9d
Autor:
Mauro Caffau
Publikováno v:
Geologija, Vol 43, Iss 2, Pp 223-234 (2000)
Externí odkaz:
https://doaj.org/article/898535c1fdfc4feb8d0881b9237c9db7
Autor:
Mauro Caffau, Mario Pleničar
Publikováno v:
Geologija, Vol 37/38, Pp 123-140 (1995)
The hippuritids species Hippuritella lapeirousei (Goldfuss, 1840), Hippuritella nabresinensis (Futterer, 1893) and Hippuritella heritschi (Kühn, 1947)vigere studied through biometrical analysis. For this purpose, the areas of three morphological cha
Externí odkaz:
https://doaj.org/article/4e5efa4f20834ccb99c9860665b8ed72
Autor:
Nevio Pugliese, Mauro Caffau
Publikováno v:
Geologija, Vol 37/38, Pp 87-121 (1995)
The stratigraphie sequence of Visogliano (Karst of Trieste) belongs to lower part of the Zolla Member of the still informal and provisional "Trieste Karst Limestone Formation" and has been attributed to Middle-Late Cenomanian. This sequence records a
Externí odkaz:
https://doaj.org/article/20ca4ae386854299830b41619ec17fdd
Autor:
Mauro Caffau, Alejandro Alberto Tassone, Federica Nasi, Massimo Zecchin, Federica Donda, Jorge Gabriel Lozano, Donaldo Mauricio Bran, Andrea Caburlotto, Emanuele Lodolo
Publikováno v:
The Holocene. 32:174-182
The spectacular water outburst occurring semi-periodically when the ice-dam formed by the external front of the Perito Moreno glacier collapses, is one of the most attracting events in the UNESCO ‘Parque Nacional Los Glaciares’ of southern Patago
Publikováno v:
Marine and Petroleum Geology. 146:105971
Publikováno v:
Earth-Science Reviews. 188:210-239
The wave-ravinement surface (WRS) is a surface of sequence-stratigraphic significance that forms in shallow-water settings during transgression. It develops progressively landward during shoreface retreat due to wave action, which erodes the substrat
Publikováno v:
Marine and Petroleum Geology. 135:105425
The interplay between high-frequency relative sea-level changes, such as those connected to late Quaternary glacio-eustasy, and regional uplift usually produces staircases of marine terraces along coastal areas. These particular settings are characte
Publikováno v:
Marine and Petroleum Geology. 133:105225
The Pliocene and Pleistocene intervals of the Neogene to Quaternary succession of the Crotone Basin, southern Italy, offer good examples of shallow-marine high-frequency sequences (fourth-order or lower rank stratigraphic frameworks) composing higher