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Abstrakty
Soft-sediment deformation structures (SSDS) are widespread in the upper part of the S. Mauro Formation (Cilento Group, Middle-Late Miocene). The succession is represented mainly by thick and very thick, massive, coarse-grained sandstones, deposited by rapid sedimentation of high-density turbidity currents. The most common SSDS are short pillars, dishes, sedimentary sills and convolutions. They occur mostly in the upper parts of sandstone beds. Vertical tubes of 4–5 cm in diameter and up to 50 cm long constitute the most striking structures. They begin in the middle part of sandstone beds, which are basically massive or contain faint dish structures. These tubes can bifurcate upwards and/ or pass into bedding-parallel veins or dikes. The vertical tubes sometimes form sand volcanoes on the then sedimentary surface. The SSDS are interpreted as the result of earthquake-triggered liquefaction and/or fluidisation of the turbidites that were affected by the seismic shocks. This implies that the deformed layers should be considered as seismites.
Czasopismo
Rocznik
Tom
Strony
67--78
Opis fizyczny
Bibliogr. 52 poz.
Twórcy
autor
- Dipartimento di Scienze e Tecnologie, Università del Sannio, Via dei Mulini 59a, 82100 Benevento, Italy
autor
- Institute of Geological Sciences, Jagiellonian University, Oleandry 2, 30-063 Krakow, Poland
autor
- Istituto per l’Ambiente Marino Costiero, CNR, Calata Porta di Massa, Porto di Napoli 83, 80133 Napoli, Italy
Bibliografia
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- Critelli, S. & Le Pera, E., 1994. Detrital modes and provenance of Miocene sandstones and modern sands of the Southern Apennines thrust-top basins (Italy). Journal of Sedimentary Research A64, 824–835.
- Dżułyński, S., 2001. Atlas of sedimentary structures from the Polish Flysch Carpathians. Institute of Geological Sciences, Jagiellonian University (Krakow), 132 pp.
- Dżułyński, S. & Walton, E.K., 1965. Sedimentary features of flysch and greywackes. Developments in Sedimentology. Elsevier (Amsterdam), 274 pp.
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- Ietto, A., Pescatore, T. & Cocco, E., 1965. Il flysch mesozoico del Cilento occidentale [The Mesozoic flysch of western Cilento]. Bollettino della Società dei Naturalisti in Napoli 74, 396–402.
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- Lowe, D.R., 1975. Water escape structures in coarse-grained sediments. Sedimentology 22, 157–204.
- Lowe, D.R., 1976. Subaqueous liquefied and fluidized sediment flows and their deposits. Sedimentology 23, 285–308.
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- Lowe, D.R. & Lo Piccolo, R.D., 1974. The characteristics and origin of dish and pillar structures. Journal of Sedimentary Petrology 44, 484–501.
- Martelli, L., Nardi, G., Bravi, S., Cavuoto, G. & Toccaceli, R.M., 2005. Note illustrative della Nuova Carta geologica d’Italia alla scala 1:50.000: Foglio 503 “Vallo della Lucania” [Notes to the new Geological Map of Italy, 1:50,000, Sheet 503 ‘Vallo della Lucania’]. Presidenza del Consiglio Dei Ministri – Dipartimento per i Servizi Tecnici Nazionali – Servizio Geologico D’Italia. S.EL.CA. (Firenze), 86 pp.
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- Mutti, E., Davoli, G., Mora, S. & Papani, L., 1994. Internal stacking patterns of ancient turbidite systems from collisional basin. [In:] P. Weimer, A. Bouma & B.F. Perkins (Eds): Submarine fans and turbidite system. GCSSEPM Foundation 15th Annual Research Conference (December 1994, Houston, Texas), 257–268.
- Mount, J.F., 1993. Formation of fluidization pipes during liquefaction: examples from the Uratanna Formation (Lower Cambrian), South Australia. Sedimentology 40, 1027–1037.
- Nichols, R.J., Sparks, R.S.J. & Wilson, C.J.N., 1994. Experimental studies of the fluidization of layered sediments and the formation of fluid escape structures. Sedimentology 41, 233–253.
- Owen, G., 1995. Soft-sediment deformation in Upper Proterozoic Torridonian sandstones (Applecross Formation) at Torridon, Northwest Scotland. Journal of Sedimentary Research A65, 495–504.
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- Pescatore, T., 1966. Strutture sedimentarie nel Flysch del Cilento occidentale [Sedimentary structures in the western Cilento flysch]. Geologica Romana 5, 99–116.
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- Russo, M., Zuppetta, A. & Guida, A., 1995. Alcune precisazioni stratigrafiche sul Flysch del Cilento (Appennino meridionale) [Some stratigraphic clarifications on the Cilento Flysch (southern Apennines)]. Bollettino della Società Geologica Italiana 114, 353–359.
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Typ dokumentu
Bibliografia
Identyfikator YADDA
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