FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W2100826001> ?p ?o ?g. }

• W2100826001 endingPage "287" @default.
• W2100826001 startingPage "1" @default.
• W2100826001 abstract "Depositional sequences and their relation to relative fluctuations in sea level is one of the main issues in present-day Eanh Sciences. The generation of depositional sequences is controlled by the interplay of tectonics, sediment supply and eustatic sea level fluctuations (e.g. Haug, 1900; Suess, 1906; Grabau, 1913; Stille, 1924; Kuenen, 1939; Krumbein and Sloss, 1956; Fisher and Brown, 1972; Frazier, 1974; Payton, 1977; Burton et aI., 1987; Cloetingh, 1988; Wilgus et aI., 1988; Galloway, 1989; Walker, 1989). In order to establish the relative importance of these factors in foreland areas, previous studies have focused on the relation between tectonic activity and facies migrations on one hand and subsidence patterns on the other (Allen, 1986; Kleinspehn and Paola, 1988; Hemmings and Jordan, 1989, 1990; Cross, 1990; Angevine et aI., 1990; Macdonald, 1991). Comparing such data with forward models created many controversies; these were probably mainly due to the variability in parameters used in geophysical models, and to the discrepancy in scale between geophysical and geological models. In the present study, detailed tectonic and stratigraphic data from the Calabrian fore-arc area (southern Italy) are used together in order to show the relations between the various parameters and their role in the genesis of depositional sequences. The Late Neogene of Central Calabria was chosen because of its interesting position along the external side of the Central Mediterranean Calabrian Arc (Finetti, 1982; Moussat, 1983; Boccaletti et aI., 1984; Mantovani et aI., 1985; Kastens et aI., 1988; Patacca and Scandone, 1989). Rapid facies changes, ranging from continental to open marine, complex tectonically-defined unconfonnities within very small sub-basins, and a wide range of phenomena reflecting syn-depositional tectonic activity were known to occur. Furthennore, there is a thick, heterogeneous pile of Messinian clastic evaporites and continental deposits, reflecting major eustatic sea level fluctuations in this time interval. During field campaigns from 1983 till 1990, a number of local geological problems related to complex stratigraphic relationships and tectonic defonnations of the area had to be overcome. Data are presented in the fonn of detailed stratigraphic colums, composite structural profJ.J.es and paleogeographical maps which display encountered reflections of syndepositional tectonics. Additional infonnation from literature includes maps of basement structure, seismic sections and borehole data. An extensive review of previous geological literature is provided." @default.
• W2100826001 created "2016-06-24" @default.
• W2100826001 creator A5070475611 @default.
• W2100826001 date "1992-10-21" @default.
• W2100826001 modified "2023-09-26" @default.
• W2100826001 title "Late neogene fore-arc basin evolution in the Calabrian arc (Central Mediterranean); tectonic sequence stratigraphy and dynamic geohistory" @default.
• W2100826001 hasPublicationYear "1992" @default.
• W2100826001 type Work @default.
• W2100826001 sameAs 2100826001 @default.
• W2100826001 citedByCount "1" @default.
• W2100826001 crossrefType "dissertation" @default.
• W2100826001 hasAuthorship W2100826001A5070475611 @default.
• W2100826001 hasConcept C109007969 @default.
• W2100826001 hasConcept C126753816 @default.
• W2100826001 hasConcept C127313418 @default.
• W2100826001 hasConcept C146588470 @default.
• W2100826001 hasConcept C151730666 @default.
• W2100826001 hasConcept C193748577 @default.
• W2100826001 hasConcept C27492601 @default.
• W2100826001 hasConcept C42907665 @default.
• W2100826001 hasConcept C77928131 @default.
• W2100826001 hasConceptScore W2100826001C109007969 @default.
• W2100826001 hasConceptScore W2100826001C126753816 @default.
• W2100826001 hasConceptScore W2100826001C127313418 @default.
• W2100826001 hasConceptScore W2100826001C146588470 @default.
• W2100826001 hasConceptScore W2100826001C151730666 @default.
• W2100826001 hasConceptScore W2100826001C193748577 @default.
• W2100826001 hasConceptScore W2100826001C27492601 @default.
• W2100826001 hasConceptScore W2100826001C42907665 @default.
• W2100826001 hasConceptScore W2100826001C77928131 @default.
• W2100826001 hasLocation W21008260011 @default.
• W2100826001 hasOpenAccess W2100826001 @default.
• W2100826001 hasPrimaryLocation W21008260011 @default.
• W2100826001 hasRelatedWork W1549428130 @default.
• W2100826001 hasRelatedWork W1968256494 @default.
• W2100826001 hasRelatedWork W1988743237 @default.
• W2100826001 hasRelatedWork W2002026394 @default.
• W2100826001 hasRelatedWork W2024109686 @default.
• W2100826001 hasRelatedWork W2051897233 @default.
• W2100826001 hasRelatedWork W2078604450 @default.
• W2100826001 hasRelatedWork W2078822248 @default.
• W2100826001 hasRelatedWork W2109934455 @default.
• W2100826001 hasRelatedWork W2145253618 @default.
• W2100826001 hasRelatedWork W2151553270 @default.
• W2100826001 hasRelatedWork W2163475804 @default.
• W2100826001 hasRelatedWork W2183793512 @default.
• W2100826001 hasRelatedWork W2271685181 @default.
• W2100826001 hasRelatedWork W2477153380 @default.
• W2100826001 hasRelatedWork W2549025592 @default.
• W2100826001 hasRelatedWork W2747484733 @default.
• W2100826001 hasRelatedWork W3128635762 @default.
• W2100826001 hasRelatedWork W2600493644 @default.
• W2100826001 hasRelatedWork W2948464229 @default.
• W2100826001 isParatext "false" @default.
• W2100826001 isRetracted "false" @default.
• W2100826001 magId "2100826001" @default.
• W2100826001 workType "dissertation" @default.