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Abstrakty
The Adriatic Sea is an epicontinental, closed sea, part of the Mediterranean. It formed in the Late Miocene, and ended structurally during the Pliocene and Quaternary, when most of its sediments were deposited. The larger Pliocene and Quaternary depressions occur mostly by the western coast, where the deposits are several thousand metres thick, and were sourced from the Alps and the Apennines. The east coast is characterised by the large and elongated Dinarides Mts., that have continental drainage extremely close to the shoreline and a very small erosional rate. Consequently, eastern inflows were and are very short, including strongly tidal estuaries that erode only small volumes of mostly carbonate detritus, adjacent to frontal islands or mountains, with restricted depositional areas. The Neretva River deposits make up part of the largest contemporary delta system on the eastern Adriatic coast, and have been analysed in this study using three seismic sections and one exploration well. These deposits are recognized inside the Neretva and Korčula channels, assuming that processes operating during Quaternary glacial phases shifted the delta tens of kilometres to the west in the past on several occasions.
Czasopismo
Rocznik
Tom
Strony
233–--241
Opis fizyczny
Bibliogr. 27 poz., rys., wykr.
Twórcy
autor
- INA-Industry of Oil Plc., Šubiæeva 29, 10000 Zagreb, Croatia
autor
- Faculty of Mining, Geology and Petroleum Engineering, Pierottijeva 6, Zagreb, Croatia
Bibliografia
- 1. Adams E.W., Schlager W., Anselmetti F.S. (2001) Morphologyand curvature of delta slopes in Swiss lakes: lessons for the interpretation of clinoforms in seismic data. Sedimentology, 48:661-679.
- 2. Balic D., Malvic T. (2011) First insights about Pliocene-Quaternary sedimentation in Neretva River palaeodelta. The First Central and Eastern European International Oil and Gas Conference and Exibition (eds. A. Holoda, M. Zelić, A. sr. Osz, J. Križ), Abstracts: 125. MoNTAN-PRESS Program Organizing, Consulting and Publishing Ltd., Budapest.
- 3. Cattaneo A., Correggiari A., Langone L., Trincardi F. (2003) The late-Holocene Gargano subaqueous delta, Adriatic shelf: sediment pathways and supply fluctuations. Marine Geology, 193: 61-91.
- 4. Colantoni P., Gallignani P., Lenaz R. (1979) Late Pleistocene and Ho i ocene evolution of the North Adriatic Shelf (Italy). Ma tine Geology, 33: M41-M50.
- 5. Correggiari A., Roveri M., Trincardi F. (1996) Late Pleistocene and Holocene evolution of the North Adriatic Sea. Quaternario, 9 (2): 697-704.
- 6. Correggiari A., Trincardi F., Langone L., Roveri M. (2001) Styles of failure in heavily-sedimented highstand prodelta wedges on the Adriatic shelf. Journal of Sedimentary Research, 71: 218-236.
- 7. Cukrov N., Suric M., Fuček L., Cosovic V., Korbar T., Juračic M. (2010) Geology of Krka Riverestuary. Proceedings of 4th Croatian Geological Congress (ed. M. Horvat): 143-148. October 14-16, 2010, Šibenik, Croatia.
- 8. Fairbanks R.G. (1989) A 17,000 year glacio-eustatic sea level record: influence of glacial melting rates on the Younger Dryas event and deep-ocean circulation. Nature, 342: 637-642.
- 9. Frignani M., Langone L. (1991) Accumulation rates and 137Cs distribution in sediments of the Po River delta and the Emilia-Romagna coast (northwestern Adriatic Sea, Italy). Continental Shelf Research, 11: 525-542.
- 10. Gensous B., Williamson D., Tesson M. (1993) Late-Quaternary transgressive and highstand depos í ts of a deltaic shelf (Rhone delta, France). IAS Special Publications, 18: 197-211.
- 11. Gotovac H., Bojanic D., Vranješ M., Jovic V., Andričevic R. (2003) Prodor mora u aluvij donje Neretve (Intrusion of sea into the lower Neretva altuvium - in Croatian). Proceedings of 3th Croatian conference about waters “Hrvatske vode u 21. stoljeću” (ed. D. Gereš): 247-254. May 28-31, 2003, Osijek, Croatia.
- 12. Kalac K. (2008) Biostratigrafsko-kronostratigrafska istraživanja pliocensko-pleistocenskih naslaga u podmorju Jadrana s posebnim osvrtom na klimatske promjene (Biostratigraphic and chronostratigraphic explorations of Pliocene-Pleistocene sediments in the Adriatic with special review of the climate changes - in Croatian). Naftaplin, book 45 (8).
- 13. Marini M., Grilli F., Guarnieri A., Jones B.H., Klaic Z., Pinardi N., Sanxhaku M. (2010) Is the southeastern Adriatic Sea coastal strip and eutrophic area? Estuarine, Coastal and Shelf Science, 88 (3): 395-406.
- 14. Milliman J.D., Syvitski J.P.M. (1992) Geomorphic/tectonic control of sediment discharge to the ocean: the importance of small mountainous rivers. Journal of Geology, 100: 525-544.
- 15. Prelogovic E., Kranjec V. (1983) Geološki razvitak podrucja Jadranskog mora. Pomorski zbornik, 21: 387-405.
- 16. Rio D., Channel J.E.T., Bertoldi R., Poli M.S., Vergerio P.R., Raffi I., Sprovieri R., Thunell R.C. (1997) Pliocene sapropels in the northern Adraiatic area: chronology and paleoenvironmental significance. Palaeogeography, Palaeoclimatology, Palaeoecol- ogy, 135: 1-25.
- 17. Sondi I., Juračic M., Pravdic V. (1995) Sedimentation in a disequilibrium river-dominated es tu ary. The Raša River Estuary (Adriatic Sea-Croatia). Sedimentology, 42: 769-782.
- 18. Sorgente D. (1999) Studio della sedimentazione attuale e recente nel medio Adriatico attraverso l'uso di traccianti radioattivi. Dissertation, University of Bologna.
- 19. Thunel M. (1971) Grada tercijarnog bazena u sjeveroistocnom dijelu Jadranskog mora (Settings of the Tertiary basin in the north-eastern part of the Adriatic Sea - in Croatian). Nafta, 22 (4-5): 275-434.
- 20. Trincardi F., Cattaneo A., Correggiari A. (2004) Mediterranean prodelta systems. Oceanography, 17 (4): 35-45.
- 21. Van Straaten L.M.J.U. (1964) Turbidite Sediments in the Southern Adriatic Sea. Developments in Sedimentology, 3: 142-147.
- 22. Velic J. (2007) Geologija ležišta nafte i plina (Geology of oil and gas reservoirs - in Croatian), first ed. University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb.
- 23. Velic J., Malvic T. (2011) Depositional conditions during Pliocene and Pleistocene in Northern Adriatic and possible lithostratigraphic division of these rocks. Nafta, 62 (1-2): 33-38.
- 24. Velic J., Velic I., Kljajo D. (2011) Sed í mentary bodies, forms and occurences in the Tudorevo and Mirovo glacial deposits of northern Velebit (Croatia). Geologia Croatica, 64 (1): 1-16.
- 25. Veseli V. (1999) Facijesi karbonatnih sedimenata mladeg mezozoika i paleogena u pucinskim bušotinama sjevernog Jadrana (Late Mesozoic and Palaeogene carbonate facies in the off-shore wells in the northern Adria - in Croatian). Dissertation, University of Zagreb, Faculty of Mining, Geology and Petroleum Engineering, Zagreb.
- 26. Vlahovic I., Tišljar J., Velic I. and Matičec D. (2005) Evolution of the Adriatic Carbonate Platform: palaeogeography, main events and depositional dynamics. Palaeogeography, Palaeoclimatology, Palaeoecology, 220 (3-4): 333-360.
- 27. Wilkinson B.H., Byrne J.R. (1977) Lavaca Bay - transgressive deltaic sedimentation in Central Texas estuary. AAPG Bulletin, 61 (4): 527-545.
Typ dokumentu
Bibliografia
Identyfikator YADDA
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