A CARBONATE RAMP EVOLUTION IN THE TRANSITION FROM THE APULIA PLATFORM TO THE IONIAN BASIN DURING EARLY TO LATE CRETACEOUS (NW GREECE)


K. Getsos
F. Pomoni-Papaioannou
A. Zelilidis
Résumé

Facies analysis of Cretaceous carbonate sequences from the external and central Ionian zone revealed a homoclinal ramp model of evolution. During Berriasian to Valanginian, the carbonate ramp was differentiated to an inner-mid and outer ramp environment, which corresponded to the external and central Ionian zone, respectively, while the main inner ramp environment is assumed that was located in the Pre-Apulian zone. The external Ionian zone (inner-mid ramp) is characterized by muds tones-wackes tones with fragmented echinoderms, bivalves, radiolarians and rare aptychus considered to be deposited below the fairweather wave base (FWWB). Locally, thin graded storm deposits intervene, indicating deposition above the storm weather wave base (SWB). Minor occurrences of packs tonesgrainstones, with fragmented echinoderms, calcareous algae, tubiphytes, lagenid foraminifera and rare ooids occur, as well, considered to be deposited at the lowermost part of the inner ramp, near the constantly agitated fairweather wave base (FWWB). The central Ionian zone (outer ramp) is mainly characterized by mudstones-wackestones with abundant radiolarians and rare calpionellids and calcispheres, considered to be deposited below the storm wave base (SWB). No talus or breccias deposits were observed, during the mentioned time interval, in any part of the studied area. From Hauterivian to Turonian, continual sea-level rise, led to establishment of outer ramp environment in the external Ionian zone, over the previous inner-mid ramp, and outer ramp-basin environment, over the previous outer ramp, in the central Ionian zone. The transition from shallower to deeper conditions is characterized by an overall deposition of mudstones-wackestones with abundant radiolarians rooted in pure micrite.
 

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  • Rubrique
  • Palaeontology, Stratigraphy and Sedimentology
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Références
Aigner, T., 1984. Dynamics of intercratonic carbonate ramps, Upper Muschelkalk, (Middle Triassic), South-German Basin, 7th Meeting of Carbonate Sedimentologists, Liverpool.
Aubouin, J., 1959. Contribution a l'étude géologique de la Grece septentrionale: les confins de l'Epire et de la Thesallie, Annales Géologique des Pays Helléniques, 10, 870-885.
Bernoulli, D., and Renz, O., 1970. Jurassic Carbonate Facies and New Ammonite Faunas from Western Greece, Eel. Geol. Hei, 63/2, 573-607.
Bornovas, J., 1961. Observations nouvelles sur la geologie des zones preapulienne et ionienne (Grece occidentale), Bull. Soc. Geol. France, series 7, II/4, 410-414.
Bosellini, Α., and Morsilli, M., 1997. A Lower Cretaceous drowning uncomformity on the eastern flank of the Apulia Platform (Gargano Promontory, southern Italy), Cretaceous Research, 18,51-61.
British Petroleum Co. Ltd. (BP), 1971. The geological results of petroleum exploration in western Greece, Instil Geol. Sub. Res., Special report 10.
Burchette, T.P., and Wright, V.P., 1992. Carbonate ramp depositional systems, Sedimentary Geology, 79, 3-57.
Calvet, and Tucker, M., 1988. Outer ramp cycles in the Upper Muschelkalk of the Catalan Basin, northern Spain, Sedimentary Geology, 57, 185-198.
Dunham, R.J., 1962. Classification of carbonate rocks according to depositional texture, Memoir, American Association of Petroleum Geologists, 1, 108-121.
Flügel, E., 1972. Mikrofazielle Untersuchungen in der Alpinen Trias. Methoden and Probleme, Mitt. Ges. Geol. Bergbaustud. 21, 9-64.
Getsos, K., Pomoni-Papaioannou, F., and Zelilidis, Α., 2004. Triassic carbonate and evaporite sedimentation in Ionian zone (western Greece): palaeogeographic and palaeoclimatic implication, Bulletin of the Geological Society of Greece, XXXVI, 699-707.
Getsos, K., Pomoni-Papaioannou, F. and Zelilidis, Α., 2005. A carbonate ramp type differentiation of the western Ionian basin during early to late Cretaceous (NWGreece), 7th international Symposium on the Cretaceous, Abstracts, 132.
Gradstein, F.M., Ogg, J.G., Smith, A.G., Bleeker, W., and Lourens, L.J., 2004. A new geologic time scale with special reference to Precambrian and Neogene, Episodes, 27, 83-100.
Graziano, R., 2000. The Aptian-Albian of the Apulia Carbonate Platform (Gargano Promontory, southern Italy): evidence of palaeoceanographic and tectonic controls on the stratigraphie architecture of the platform margin, Cretaceous Research, 21, 107-126.
Haq, B.U., Hardenbol, J., and Vail, P.R., 1987. Chronology of Fluctuating Sea Levels Since the
Triassic, Science, 235, 1156-1167.
IGRS-IFP, 1966. Etude gélogique de l'Epire (Grece nordoccidentale), Ed. Technip, Paris, 306pp.
Karakitsios, V., 1990. Study of Jurassic age paleofaults in Ionian zone (Epirus, Greece), Proceedings of the 5th international Congress, XXV/1,307-318.
Karakitsios, V., 1992. Ouverture et inversion tectonique du basin ionien (Epire, Grece). Annales Géologique des Pays Helléniques, 35, 85-318.
Karakitsios, V., and Tsaila-Monopolis, S., 1988. Données nouvelles sur les niveaux supérieurs (Lias inférieur - moyen) des calcaires de Pantokrator (Zone Ionienne moyen, Epire, Grece contenentale) description des calcaires de Louros (New data from the upper part (early middle Lias) of the Pantokrator limestone (middle Ionian zone, Epirus, continental Greece) description of Louros limestone), Rev. de Micropaleontologie, 31(1), 49-55.
Karakitsios, V., Danelian, T., and De Wever, P., 1988. Datation par les radiolaires des Calcaires ä Filaments, Schists a Posidonies supérieurs et Calcaires de Vigla "zone Ionienne, Epire, Grèce", du Callovient au Tithonique terminal, Compte Rendu de l'Académie des Sciences, 306/11, 367-372.
Karakitsios, V., and Koletti, L., 1992. Critical revision of the age of the basal Vigla limestones (Ionian zone, western Greece), based on nannoplankton and calpionellids with paleogeographical consequences. In B. Hamrsmid and J. Young (eds), Proceedings of the Forth International Nannoplankton Association Conference, Prague, 1991, Knihovnicka ZPN, 14a, vol. l,p. 165-177.
Karakitsios, V., Tsikos, H., Van Breugel, Y., Bakopoulos, L, and Koletti, L., 2004. Cretaceous oceanic anoxie events in western continental Greece, Bull of the Geol. Soc. Greece, XXXVI, 846-855.
Pomoni, F., 1983. Studiul pétrographie si sedimentologie al evaporitelor Triasice din regiunea Epir, Teza de Doctorat, Universitatea Bucuresti, l-190pp.
Pomoni-Papaioannou, F., 1985. The sedimentology and depositional environment of the Triassic dolomite-gyprum facies of western Greece, Proceedings of the 6th European Meeting of the Inter. Assoc. Sedimentologists, 367-368.
Pomoni-Papaioannou, F., Karakitsios, V., Kamberis, E., and Marneiis, F., 2004. Chevron-type halite and nodular anhydrite in the Triassic Evaporitic Formation of the Ionian Zone (Western Greece), Proceedings of the 10th International Congress,Bulletin of the Geological Society of Greece, XXXVI, 578-586.
Renz, C, 1955. Die vorneogene Stratigraphie der normal-sedimentaren Formationen Griechenlan, Inst. Geol. Susururf Res. Athens, 637.
Underhill, J.R., 1989. Late Cenozoic deformation of the Hellenide foreland, western Greece, Geological Society of America, Bulletin, 101, 613-634. Wilson, J.L., 1975. Carbonate Facies in Geologic History, Berlin-Heidelberg-New York (Springer), 47 lp.
Zelilidis, Α., Piper, D. J., Vakalas, I., Avramidis, P., and Getsos, K., 2003. Oil and Gas Plays in Albania: Do Equivalent Plays Exist in Greece? Journal of Petroleum Geology, 26, 29-48.
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