Depositional environments of tertiary turbiditic sediments in Metsovo Basin, NW Greece


Published: Aug 1, 2018
Keywords:
Metsovo basin submarine fan turbidites sole marks
G. ANANIADIS
A. ZELILIDIS
Abstract

Tertiary sediments in Metsovo area consist of submarine fan turbidite deposits accumulated in the proximal part of the basin and represent mostly inner fan. The most proximal part of the inner fan could be related to a shelf environment. Palaeocurrent data indicate mainly two directions. The main direction is SW and results mainly from groove marks. The second direction represents an WNW trend which results mainly from flute marks. The Metsovo area seems to have multiple feeders from North and East. The total thickness of the turbiditic deposits in Metsovo area is approximately 6800 m due to tectonic stacking and folding.

Article Details
  • Section
  • Sedimentology
Downloads
Download data is not yet available.
References
AUBOUIN, J., 1959. Contribution à Γ étude géologique de la Grèce septentrionale: les confins de l'Epire et de la Thessalie: Ann. Géol. des Pays Hell., 10, 1-184.
AUBOUIN, J., 1964. Reflection sur le problème des Flyschs et des Molasses: son aspect das les Hellènides (Grèce.):Eclogae Geolologicae Helvetiae,51, 451-496.
AUBOUIN, J. 1965. Geosynclines. Amsterdam: Elsevier, 350 pp.
BONORINO, G. 1996, Foreland sedimentation and plate interaction during closure of the Tethys ocean (Tertiary; Hellenides; Western Continental Greece). Journal of Sedimentary Research, 66, 1148-1155.
BOUMA, A. H. 1962. The sedimentology of some Flysch deposits: a graphic approach to fades interpretation. Amsterdam: Elsevier, 168 pp.
FLEURY, J. 1980. Les zones de Gavrovo-Tripolitza et du Pinde-Olonus (Grece occidentale et Péloponnèse du Nord): evolution d'une plateforme et d'une bassin dans leur cadre alpin. Société Géologique du Nord 4, 1-651.
JONES, G., DEWEVER, P. & ROBERTSON, A.H.F 1992. Significance of radiolarian age data to the Mesozoic tectonic and sedimentary evolution of the nothern Pindos Mountains, Greece. Geological Magazine, 129, 385- 400.
KATSIAVRIAS, N. 1983. The North Pindos Flysch : Flysch of the western part of the Gavrovo ridge . Northwestern Greece. Inst. Geol. Min. Expl., 126-139.
KOCH, Κ. E. & NICOLAUS, H. J., 1969, Zur Geologie des ostpindos flysch beckens und seiner Umrandung. Inst. for. Geol. Subsurf. Reser. Athens, raport no 9.
LORSONG, J. Α., 1977, Stratigraphy of the Pindos flysch in the Politses mountains, Northwestern Greece. VI Coll. Aegean region, II, 703-714.
RICCI LUCCHI, F. 1975.Depositional cycles in two turbidite formations of Nothern Apennines (Italy). Journal of Sedimentary Petrology, 45, 3-432.
RICHTER, D., 1993, Die Flyschzonen Griechenlands VII. Sedimentstrukturen, Ablagerungsart und Schüttungsrichtungen im Flysch der Pindos-Zone (Griechenland): N. Jahrbuch für Geol. und Paläont., Monatshefte 9, 513-544.
RICHTER,D., MULLER, C, AND MIHM, Α., 1993, Die Flyschzonen Griechenlands V. Zur Stratigraphie des Flysches der Pindos -Zone im nordlichen Pindos-Gebirge zwischen der albanischen Grenze und der Querzone von Kastaniotikos (Griechenland):. Jahrbuch für Geol. Paläont., Monatshefte, 5, 257-291.
ROBERTSON, A. H. F., CLIFT, P. D., DEGNAN, P. J. & JONES, G. 1991. Palaeogeographic and palaeotectonic evolution of the Eastern Mediterranean Neotethys. Palaeogeography, Palaeoclimatology, Palaeoecology, 87, 289-343.
STOW, D. A. V, READING, H. G. & COLLINSON, J. D. 1996. Deep Seas. In Sedimentary' Environments (éd. H. G. Reading), 395-453.
Most read articles by the same author(s)