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Olistostromes of the Pieniny Klippen Belt, Northern Carpathians

Published online by Cambridge University Press:  25 July 2014

JAN GOLONKA ,
MICHAŁ KROBICKI ,
ANNA WAŚKOWSKA ,
MAREK CIESZKOWSKI  and
ANDRZEJ ŚLĄCZKA
JAN GOLONKA*
Affiliation:
AGH University of Science and Technology, Faculty of Geology, Geophysics and Environmental Protection, Mickiewicza 30, 30-059 Kraków, Poland
MICHAŁ KROBICKI
Affiliation:
AGH University of Science and Technology, Faculty of Geology, Geophysics and Environmental Protection, Mickiewicza 30, 30-059 Kraków, Poland Polish Geological Institute – National Research Institute, Upper Silesian Branch, Królowej Jadwigi 1, 41-200 Sosnowiec, Poland
ANNA WAŚKOWSKA
Affiliation:
AGH University of Science and Technology, Faculty of Geology, Geophysics and Environmental Protection, Mickiewicza 30, 30-059 Kraków, Poland
MAREK CIESZKOWSKI
Affiliation:
Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, 30-376 Kraków, Poland
ANDRZEJ ŚLĄCZKA
Affiliation:
Jagiellonian University, Institute of Geological Sciences, Oleandry 2a, 30-376 Kraków, Poland
*
†Author for correspondence: jgolonka@agh.edu.pl
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Abstract

The olistostromes form two belts within the Pieniny Klippen Belt (PKB) in the Northern Carpathians. They mark an early stage of the development of the accretionary prism. The first belt was formed during Late Cretaceous time as a result of subduction of the southern part of the Alpine Tethys. The fore-arc basin originated along this subduction zone, with synorogenic flysch deposits. Huge olistoliths deposited within the Cretaceous–Palaeogene flysch of the Złatne Basin, presently located in the vicinity of the Haligovce village (eastern Slovakia), provide a good example of the fore-arc olistostrome setting. The second belt is related to the movement of the accretionary prism, which overrode the Czorsztyn Ridge during Late Cretaceous–Paleocene time. The destruction of this ridge led to the formation of submarine slumps and olistoliths along the southern margin of the Magura Basin. The Upper Cretaceous – Paleocene flysch sequences of the Magura Basin constitute the matrix of olistostromes. The large Homole block in the Jaworki village represents the best example of the Magura Basin olistolith. Numerous examples of olistoliths were documented in western Slovakia, Poland, eastern Slovakia and Ukraine. The olistostromes formed within the Złatne and Magura basins orginated during the tectonic process, forming the olistostrome belts along the strike of the PKB structure.

Keywords

olistolitholistostromeflyschPieniny Klippen BeltCarpathiansplate tectonics
Type
Original Articles
Information
Geological Magazine , Volume 152 , Issue 2 , March 2015 , pp. 269 - 286
Copyright
Copyright © Cambridge University Press 2014 

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References

Abbate, E., Bortolotti, V. & Sagri, M. 1981. Excursion N° 5: Olistostromes in the Oligocene Macigno formation (Florence area). Introduction: An approach to olistostrome interpretation. In Excursion Guidebook (ed. Ricci Lucchi, F.), International Association of Sedimentologists, 2nd European Regional Meeting, Bologna, 1981, pp. 165–85. Tecnoprint, Bologna.Google Scholar
Abbate, E. & Sagri, M. 1970. The eugeosynclinal sequences. Sedimentary Geology 4, 251–340.Google Scholar
Andrusov, D. 1945. Geological investigations of the inner Klippen Belt in the Western Carpathians. Part IV – Stratigraphy of Dogger and Malm, Part V – Stratigraphy of the Cretaceous. Práce Štátneho Geologického ústavu, 13, Bratislava, pp. 1–176 (in Slovak).Google Scholar
Bailey, R. H., Skehan, J. W., Dreier, R. B. & Webste, M. J. 1989. Olistostromes of the Avalonian terrane of southeastern New England. In Mélanges and Olistostromes of the U.S. Appalachians (eds Horton, J. W. J. & Rast, N.), pp. 93–112. The Geological Society of America, Special Paper no. 228.Google Scholar
Balance, P. F. 1991. Gravity flows and rock recycling on the Tonga landward trench slope: relation to trench-slope tectonic processes. Journal of Geology 99, 817–27.CrossRefGoogle Scholar
Barber, A. J., Yjokrosapoetro, S. & Charlton, T. R. 1986. Mud volcanoes, shale diapirs, wrench faults and melanges in accretionary complexes, Eastern Indonesia. AAPG Bulletin 70, 1729–41.Google Scholar
Beer, M. A. & Shcherba, I. G. 1984. The Late Alpine evolution of the Eastern Carpathians. International Geology Review 26, 765–78.CrossRefGoogle Scholar
Bill, M. L., O’Dogherty, J., Guex, P. O., Baumgartner, P. O. & Masson, H. 2001. Radiolarite ages in Alpine-Mediterranean ophiolites: constraints on the oceanic spreading and the Tethys-Atlantic connection. Geological Society of America Bulletin 113, 129–43.Google Scholar
Birkenmajer, K. 1959. Significance of the Haligovce Klippe for the geology of the Pieniny Klippen Belt (Carpathians). Rocznik Polskiego Towarzystwa Geologicznego 29 (1), 73–88 (in Polish with English summary).Google Scholar
Birkenmajer, K. 1963. Stratigraphy and paleogeography of the Czorsztyn Series (Pieniny Klippen Belt, Carpathians) in Poland. Studia Geologica Polonica 9, 1–380 (in Polish with English summary).Google Scholar
Birkenmajer, K. 1970. Przedeoceńskie struktury fałdowe w pienińskim pasie skałkowym Polski. (Pre-Eocene fold structures in the Pieniny Klippen Belt (Carpathians) of Poland.) Studia Geologica Polonica 31, 1–77 (in Polish with English summary).Google Scholar
Birkenmajer, K. 1977. Jurassic and Cretaceous lithostratigraphic units of the Pieniny Klippen Belt, Carpathians, Poland. Studia Geologica Polonica 45, 1–159.Google Scholar
Birkenmajer, K. & Lorenc, M. W. 2008. Lower Cretaceous exotic intraplate basaltoid olistolith from Biała Woda, Pieniny Klippen Belt, Poland: geochemistry and provenance. Studia Geologica Polonica 131, 237–46.Google Scholar
Birkenmajer, K. & Pécskay, Z. 2000. Early Cretaceous K–Ar age of a large basalt olistolith at Biała Woda, Pieniny Klippen Belt, West Carpathians, Poland. Studia Geologica Polonica 117, 27–35.Google Scholar
Buldygerov, V. V. & Krainov, M. A. 2012. Postcambrian stratified rocks of the northern part of the Baikal-Vitim fold area. Stratigraphy and Geological Correlation 20, 405–16.Google Scholar
Camerlenghi, A. & Pini, G. A. 2009. Mud volcanoes, olistostromes and Argille scagliose in the Mediterranean region. Sedimentology 56, 319–65.Google Scholar
Chanier, F. & Ferrière, J. 1991. From a passive margin to an active margin: tectonic and sedimentaryprocesses linked to the birth of an accretionary prism (Hikurangi margin, New Zealand). Bulletin Société Géologique de la France 162, 649–60.Google Scholar
Chrustek, M., Golonka, J., Janeczko, A. & Stachyrak, F. 2005. Geological characterisation of the Krynica Subunit in the vicinity of Krościenko on the Dunajec river (Magura Nappe, Outer Flysch Carpathians). Kwartalnik AGH, Geologia 31, 127–44.Google Scholar
Cieszkowski, M., Golonka, J., Krobicki, M., Malata, E., Olszewska, B., Oszczypko, N. & Tłuczek, D. 2004. Pozycja geologiczna utworów węglanowych we fliszu jednostki złatniańskiej rejonu Haligowiec (pieniński pas skałkowy). In Egzotyki Karpackie: Znaczenie w Rekonstrukcjach Paleogeograficznych, Ogólnopolske seminarium, 13 December 2004 (ed. Krobicki, M.), pp. 51–2. Kraków (in Polish).Google Scholar
Cieszkowski, M., Golonka, J., Krobicki, M., Ślączka, A., Oszczypko, N., Waśkowska, A. & Wendorff, M. 2009. The Northern Carpathians plate tectonic evolutionary stages and origin of olistoliths and olistostromes. Geodynamica Acta 22(1–2), 1–26.Google Scholar
Cieszkowski, M., Golonka, J., Ślączka, A. & Waśkowska, A. 2012. Role of the olistostromes and olistoliths in tectonostratigraphic evolution of the Silesian Basin in the Outer West Carpathians. Tectonophysics 568, 248–65.CrossRefGoogle Scholar
Delteil, J., Mercier De Lepinay, B., Morgans, H. E. G. & Field, B. D. 2006. Olistostromes marking tectonic events, East Coast, New Zealand. New Zealand Journal of Geology and Geophysics 49, 571–31.Google Scholar
Dominguez, S., Lallemand, S. E., Malavieille, J. & von Huene, R. 1998. Upper plate deformation associated with seamount subduction. Tectonophysics 293, 207–24.Google Scholar
Duperret, A., Bourgois, J., Lagabrielle, Y. & Suess, E. 1995. Slope instability at an active continental margin: large-scale polyphase submarine slides along the Peruvian margin, between 5°S and 6°S. Marine Geology 122, 303–28.CrossRefGoogle Scholar
Festa, A., Pini, G. A., Dilek, Y. & Codegone, G. 2010a. Mélanges and mélange-forming processes: a historical overview and new concepts. International Geology Review 52, 1040–105.Google Scholar
Festa, A., Pini, G. A., Dilek, Y., Codegone, G., Vezzani, L., Ghisetti, F., Lucente, C. C. & Ogata, K. 2010b. Peri-Adriatic mélanges and their evolution in the Tethyan realm. International Geology Review 52, 369–406.CrossRefGoogle Scholar
Flores, G. 1959. Evidence of slump phenomena (Olistostromes) in areas of hydrocarbon exploration in Sicily. In Proceedings 5th World Petroleum Congress. Roma, Section 1, 13, 259 pp.Google Scholar
Golonka, J. 2011. Evolution of the Outer Carpathian Basins. In Integrating Microfossil Records from the Oceans and Epicontinental Seas (eds Bąk, M., Kaminski, M. A. & Waśkowska, A.), pp. 3–14. Grzybowski Foundation, Special Publication no. 17.Google Scholar
Golonka, J. & Bocharova, N. Y. 2000. Hot spots activity and the break-up of Pangea. Palaeogeography, Palaeoclimatology, Palaeoecology 161, 49–69.Google Scholar
Golonka, J., Cieszkowski, M., Waśkowska, A., Krobicki, M. & Ślączka, A. 2010. Olistostromes of the Pieniny Klippen Belt, Northern Carpathians. Geologica Balcanica 39, 137–8.Google Scholar
Golonka, J., Gahagan, L., Krobicki, M., Marko, F., Oszczypko, N. & Ślączka, A. 2006. Plate tectonic evolution and paleogeography of the circum-carpathian region. In The Carpathians and their Foreland: Geology and Hydrocarbon Resources (eds Golonka, J. & Picha, F.). American Association of Petroleum Geologists, Memoir no. 84, 11–46.Google Scholar
Golonka, J. & Krobicki, M. 2004. Jurassic paleogeography of the Pieniny and Outer Carpathian basins. Rivista Italiana di Paleontologia e Stratigrafia 110 (1), 5–14.Google Scholar
Golonka, J., Krobicki, M., Oszczypko, N., Ślączka, A. & Słomka, T. 2003. Geodynamic evolution and palaeogeography of the Polish Carpathians and adjacent areas during Neo-Cimmerian and preceding events (latest Triassic–earliest Cretaceous). In Tracing Tectonic Deformation Using the Sedimentary Record (eds McCann, T. & Saintot, A.), pp. 138–58. Geological Society, London, Special Publication no. 208.Google Scholar
Golonka, J., Krobicki, M., Waśkowska-Oliwa, A., Vašíček, Z. & Skupien, P. 2008. Główne elementy paleogeograficzne Zachodnich Karpat zewnętrznych w późnej jurze i wczesnej kredzie. (Main paleogeographical elements of the West Outer Carpathians during Late Jurassic and Early Cretaceous times.) In Utwory Przełomu Jury i Kredy w Zachodnich Karpatach Fliszowych Polsko-Czeskiego Pogranicza (ed. Krobicki, M.), pp. 61–72. Geologia, Kwartalnik AGH, 34(3/1) (in Polish with English summary).Google Scholar
Golonka, J., Oszczypko, N. & Ślączka, A. 2000. Late Carboniferous Neogene geodynamics and paleogeography of the circum-Carpathian region and adjacent area. Annales Societatis Geologorum Poloniae 70, 107–36.Google Scholar
Golonka, J. & Rączkowski, W. 1984. Arkusz Piwniczna. Szczegółowa map geologiczna Polski 1:5000. Detailed Geological Map of Poland: Geological Institute, Publishing House Wydawnictwa Geologiczne, Warszawa.Google Scholar
Golonka, J. & Sikora, W. 1981. Mikrofacje ścienionych sedymentacyjnie utworów jury i kredy dolnej pienińskiego pasa skałkowego w Polsce. (Microfacies of the Jurassic and Lower Cretaceous sedimentarily thinned deposits of the Pieniny Klippen Belt in Poland.) Biuletyn Instytutu Geologicznego 331, 7–37 (in Polish with English abstract).Google Scholar
Hsü, K. J. 1974. Melanges and their distinction from olistostromes. In Modern and Ancient Geosynclinal Sedimentation (eds Dott, R. H. Jr. & Shave, R. H.), pp. 321–33. SEPM, Special Publication no. 19.Google Scholar
Hsü, K. J. 1975. Paleoceanography of the Mesozoic Alpine Tethys. Geology 3, 347–8.Google Scholar
Jurewicz, E. 1997. The contact between the Pieniny Klippen Belt and Magura Unit (the Małe Pieniny Mts). Geological Quarterly 41 (3), 315–26.Google Scholar
Jurewicz, E. 2005. Geodynamic evolution of the Tatra Mts and the Pieniny Klippen Belt (Western Carpathians): problems and comments. Acta Geologica Polonica 3, 295–338.Google Scholar
Köhler, E., Salaj, J. & Buček, S. 1993. Paleogeographical development of the Myjava sedimentary area (western Slovakia) during the existence of the Paleocene reef complex. Geologica Carpathica 44, 373–80.Google Scholar
Krobicki, M., Budzyń, B., Golonka, J., Kruglov, S., Malata, E., Michalik, M., Oszczypko, N., Skiba, M., Słaby, E., Słomka, T. & Zych, B. 2005 a. Petrography and mineralogy of the Late Jurassic – Early Cretaceous volcanic rocks in the Ukrainian part of the Carpathians. Mineralogical Society of Poland – Special Papers 25, 323–8.Google Scholar
Krobicki, M., Cieszkowski, M., Golonka, J., Kołodziej, B., Malata, E., Olszewska, B., Oszczypko, N. & Tłuczek, D. 2005 b. Koralowo-glonowe wapienie paleocenu w obrębie paleogeńskiego fliszu rejonu Haligowiec (pieniński pas skałkowy, Słowacja). In Wapienie Organogeniczne i Organodetrytyczne w Karpatach Zewnętrznych i ich znaczenie Dla Rekonstrukcji Paleogeograficznych Tetydy (eds Cieszkowski, M. & Golonka, J.), 19–21. Seminarium naukowe, 21 April 2005, Kraków (in Polish).Google Scholar
Krobicki, M. & Golonka, J. 2008 a. Geological history of the Pieniny Klippen Belt and Middle Jurassica black shales as one of the oldest deposits of this region – stratigraphical position and palaeoenvironmental significance. Geoturystyka 2 (13), 3–18.Google Scholar
Krobicki, M. & Golonka, J. 2008 b. Geotouristical values of the Pieniny Klippen Belt and Tatra Mountains regions (Poland). Przegląd Geologiczny 56, 670–9.Google Scholar
Krobicki, M., Golonka, J., Kołodziej, B., Olszewska, B., Oszczypko, N., Słomka, T., Tragelehn, H. & Wieczorek, J. 2004. Paleoceńskie olistolity wapieni koralowo-glonowych rejonu Haligowiec (pieniński pas skałkowy, Słowacja). In Egzotyki Karpackie – Znaczenie w Rekonstrukcjach Paleogeograficzno-Geotektonicznych (ed. Krobicki, M.), pp. 53–5. Ogólnopolskie seminarium, 13 December 2004, Kraków (in Polish).Google Scholar
Krobicki, M., Golonka, J. & Słomka, T. 2010. Latest Jurassic – earliest Cretaceous mass movements in the Polish part of the Pieniny Klippen Belt and Silesian Unit (Outer Flysch Carpathians). Scientific Annals, School of Geology, Aristotle University of Thessaloniki. Proceedings of the XIX CBGA Congress, Thessaloniki, Greece, Special volume 100, 209–219.Google Scholar
Krobicki, M., Kruglov, S.S., Matyja, B. A., Wierzbowski, A., Aubrecht, R., Bubniak, A. & Bubniak, I. 2003. Relation between Jurassic klippen successions in the Polish and Ukrainian parts of the Pieniny Klippen Belt. Mineralia Slovaca 35 (1), 56–8.Google Scholar
Krobicki, M., Oszczypko, N., Salata, D. & Golonka, J. 2008. Intra-plate alkaline volcanism in the Pieniny Klippen Belt (Eastern Carpathians, Ukraine). In SlovTec 8, 6th Meeting of the Central European Tectonic Studies Group (CETeG) & 13th Meeting of the Czech Tectonic Studies Group (ÈTS) (eds Z. Németh & D. Plašienka), pp. 73–4. Proceedings and Excursion Guide, Bratislava, 23–26 April 2008 Upohlav, Pieniny Klippen Belt, Slovakia.Google Scholar
Krobicki, M. & Wierzbowski, A. 2004. Pozycja stratygraficzna i paleogeograficzne znaczenie bajoskich wapieni krynoidowych w ewolucji pienińskiego basenu skałkowego. Tomy Jurajskie 2, 69–82 (in Polish with English abstract).Google Scholar
Lashkevitsch, Z. M., Medvedev, A. P. & Krupskiy, Y. Z. 1995. Tectonomagmatic Evolution of Carpathians (in Russian). Kiev: Naukova Dumka, 113 pp.Google Scholar
Lewandowski, M., Krobicki, M., Matyja, B. A. & Wierzbowski, A. 2005. Palaeogeographic evolution of the Pieniny Klippen Basin using stratigraphic and palaeomagnetic data from the Veliky Kamenets section (Carpathians, Ukraine). Palaeogeography, Palaeoclimatology, Palaeoecology 216, 53–72.Google Scholar
Lexa, J., Bezák, V., Elečko, M., Mello, J., Polák, M., Potfaj, M. & Vozár, J. (eds) 2000. Geological Map of Western Carpathians and Adjacent Areas 1:500 000. Ministry of the Environment of Slovak Republic, Geological Survey of Slovak Republic, Bratislava.Google Scholar
Lucente, C. C. & Pini, G. A. 2003. Anatomy and emplacement mechanism of a large submarine slide within the Miocene foredeep in the Northern Apennines, Italy: A field perspective. American Journal of Science 303, 565–602.Google Scholar
Lucente, C. C. & Pini, G. A. 2008. Basin-wide mass-wasting complexes as markers of the Oligo-Miocene foredeep-accretionary wedge evolution in the Northern Apennines, Italy. Basin Research 20, 49–71.CrossRefGoogle Scholar
McAdoo, B. G., Pratson, L. F. & Orange, D. L. 2000. Submarine landslide geomorphology, US continental slope. Marine Geology 169, 103–36.Google Scholar
Mello, J. (ed.) 2005. Geological map of the middle Váh Valley region 1:50000. MŽP – ŠGÚDŠ, Bratislava.Google Scholar
Mosher, D. C., Shipp, R. C., Moscardelli, L., Chaytor, J. D., Baxter, C. D. P., Lee, H. J. & Urgeles, R. (eds) 2010. Submarine mass movements and their consequences. 4th International Symposium on Advances in Natural and Technological Hazards Research, vol. 28. Dodrecht: Springer, 786 pp.Google Scholar
Nemčok, J. 1980. Non-traditional view of East-Slovakian Klippen Belt. Geologický Zbornik Geologica Carpa-thica 31, 563–8.Google Scholar
Neuendorf, K. E., Mehl, J. P. Jr. & Jackson, J. R. (eds) 2005. Glossary of Geology, 5th edition. Berlin: Springer Verlag, 779 pp.Google Scholar
Neumayr, M. 1871. Jurastudien. Der penninische Klippenzug. Jahrbuch der Kaiserlich-Königlichen Geologischen Reichanstalt 21, 451–536.Google Scholar
Oszczypko, N., Jurewicz, E. & Plašienka, D. 2010. Tectonics of the Klippen Belt and Magura Nappe in the eastern part of the Pieniny Mts (Western Carpathians, Poland and Slovakia) – new approaches and results. Scientific Annals, School of Geology, Aristotle University of Thessaloniki. Proceedings of the XIX CBGA Congress, Thessaloniki, Greece, Special volume 100, 221–9.Google Scholar
Oszczypko, N., Oszczypko-Clowes, M., Golonka, J. & Krobicki, M. 2005 a. Position of the Marmarosh Flysch (Eastern Carpathians) and its relation to the Magura Nappe (Western Carpathians). Acta Geologica Hunga-rica 48 (3), 259–82.Google Scholar
Oszczypko, N., Oszczypko-Clowes, M., Golonka, J. & Marko, F. 2005 b. Oligocene – Lower Miocene sequences of the Pieniny Klippen Belt and adjacent Magura Nappe between Jarabina and the Poprad River (East Slovakia and South Poland): their tectonic position and paleogeographic implications. Geological Quarterly 49, 379–402.Google Scholar
Oszczypko, N., Salata, D. & Krobicki, M. 2012. Early Cretaceous intra-plate volcanism in the Pieniny Klippen Belt – a case study of the Velykyi Kamenets’/Vilkhivchyk (Ukraine) and the Biała Woda (Poland) sections. Geological Quarterly 56 (4), 629–48.Google Scholar
Pieńkowski, G., Schudack, M. E., Bosák, P., Enay, R., Feldman-Olszewska, A., Golonka, J., Gutowski, J., Herngreen, G. F. W., Jordan, P., Krobicki, M., Lathuiliere, B., Leinfelder, R. R., Michalík, J., Mönnig, E., Noe-Nygaard, N., Pálfy, J., Pint, A., Rasser, M. W., Reisdorf, A. G., Schmid, D. U., Schweigert, G., Surlyk, F., Wetzel, A. & Wong, T. E. 2008. Jurassic. In The Geology of Central Europe, vol. 2, Mesozoic and Cenozoic (ed. McCann, T.), pp. 823–922. London: Geological Society.Google Scholar
Pini, G. A. 1999. Tectonosomes and olistostromes in the Argille Scagliose of the Northern Apennines, Italy. Geological Society of America Special Paper 335, 1–73.Google Scholar
Pini, G. A., Camerlenghi, A., Ogata, K., Festa, A., Codegone, G., Lucente, C. C. & Urgeles, R. 2010. Olistostromes, mélanges and mass-transport deposits. Rendiconti Online Societa Geologica Italiana 11, 445–6.Google Scholar
Plašienka, D. 2012. Jurassic syn-rift and Cretaceous syn-orogenic, coarse-grained deposits related to opening and closure of the Vahic (South Penninic) Ocean in the Western Carpathians – an overview. Geological Quarterly 56 (4), 601–28.Google Scholar
Plašienka, D., Sýkora, M., Aubrecht, R., Krobicki, M. & Józsa, S. 2010. Reinterpretation of the lithostratigraphy and tectonic position of the Mariková Klippen (Middle Váh Valley, western Slovakia). Acta Geologica Slovaca 2 (1), 1–9.Google Scholar
Potfaj, M. 2002. The saddle between Haligovce and Lesnica. Guide to geological excursions. XIIth Congress Carpathian-Balkan Geological Association, Bratislava, Slovak Republic, appendix, pp. 1–4.Google Scholar
Reháková, D., Matyja, B. A., Wierzbowski, A., Schlögl, J., Krobicki, M. & Barski, M. 2011. Stratigraphy and microfacies of the Jurassic and lowermost Cretaceous of the Veliky Kamenets section (Pieniny Klippen Belt, Carpathians, Western Ukraine). Volumina Jurassica 9, 61–104.Google Scholar
Ricci Lucchi, F. 1986. The Oligocene to Recent foreland basins of the northern Apennines. In Foreland Basin (eds Allen, P. A. & Homewood, P.), pp. 105–40. International Association of Sedimentologists, Special Publication no. 8.Google Scholar
Richter, D. 1973. Olisthostrom, Olistholit, Olisthorymma und Olisthoplaka als Merkmale von Gleistungs- und Resedimentationsvorgangen infolge synsedimentarer tectogenetischer Bewengungen in Geosynklinalbereichen. Neues Jahrbuch für Geologie und Palaeontologie Abhandlungen 143 (3), 304–44.Google Scholar
Salaj, J. 1991. Biostratigraphic correlation of Cretaceous flysch formations in the Klippen and Peri-Klippen zones of the Middle Váh valley and their paleogeographic-tectonic history. Mineralia Slovaca 23, 295–313 (in Slovak with English abstract).Google Scholar
Schmid, S. M., Bernoulli, D., Fugenschuh, B., Matenco, L., Schefer, S., Schuster, R., Tischler, M. & Ustaszewski, K. 2008. The Alpine-Carpathian-Dinaridic orogenic system: correlation and evolution of tectonic units. Swiss Journal of Geosciences 101, 139–83.Google Scholar
Shcherba, I. G. 1979. Pliocene-Quaternary olistostromes of Crimea and mechanism of their formation. International Geology Review 21, 1140–8.Google Scholar
Sikora, W. 1971. Esquisse de la tectogenèse de la zone des Klippes des Pieniny en Pologne d’après de nouvelles données géologiques. Rocznik Polskiego Towarzystwa Geologicznego 41 (1), 221–39.Google Scholar
Ślączka, A., Kruglov, S., Golonka, J., Oszczypko, N. & Popadyuk, I. 2006. The General Geology of the Outer Carpathians, Poland, Slovakia, and Ukraine. In The Carpathians and their Foreland: Geology and Hydrocarbon Resources (eds Golonka, J. & Picha, F.),Ricci pp. 221–58. American Association of Petroleum Geologists, Memoir no. 84.Google Scholar
Ślączka, A., Renda, P., Cieszkowski, M., Golonka, J. & Nigro, F. 2012. Sedimentary basins evolution and olistoliths formation: The case of Carpathian and Sicilian regions. Tectonophysics 568, 306–19.Google Scholar
Varitchev, A. 1997. Major and trace element geochemistry of Mesozoic igneous formation of the Ukrainian Carpathians as an indicator of paleotectonic settings. Przegląd Geologiczny 45, 1109–10.Google Scholar
von Huene, R. & Lallemand, S. 1990. Tectonic erosion along the Japan and Peru convergent margins. Geological Society of America Bulletin 102, 704–20.Google Scholar
von Huene, R., Raner, C. & Watts, T. 2004. Tsunamigenic slope failure along the Middle America Trench in two tectonic settings. Marine Geology 203, 303–17.Google Scholar
von Huene, R. & Scholl, D. W. 1991. Observations at convergent margins concerning sediment subduction, subduction erosion, and the growth of continental crust. Reviews of Geophysics 29, 279–316.Google Scholar
Wendorff, M. 2003. Stratigraphy of the Fungurume Group - evolving foreland basin succession in the Lufilian fold-thrust belt, Neoproterozoic-Lower Palaeozoic, Democratic Republic of Congo. South African Journal of Geology 106, 17–34.Google Scholar
Wendorff, M. 2005. Lithostratigaphy of Neoproterozoic syn-rift sedimentary megabreccia from Mwambashi, Copperbelt of Zambia, and correlation with olistostrome succession from Mufulira. South African Journal of Geology 108, 505–24.Google Scholar
Wierzbowski, A., Aubrecht, R., Krobicki, M., Matyja, B. A. & Schlögl, J. 2004. Stratigraphy and palaeogeographic position of the Jurassic Czertezik Succession, Pieniny Klippen Belt (Western Carpathians) of Poland and Eastern Slovakia. Annales Societatis Geologorum Poloniae 74, 237–56.Google Scholar
Wierzbowski, A., Jaworska, M. & Krobicki, M. 1999. Jurassic (Upper Bajocian-lowest Oxfordian) ammonitico rosso facies in the Pieniny Klippen Belt, Carpathians, Poland: its fauna, age, microfacies and sedimentary environment. Studia Geologica Poloniae 115, 7–74.Google Scholar
Yamada, Y., Kawamura, Y., Ikehara, K., Ogawa, Y., Urgeles, R., Mosher, D., Chaytor, J. & Strasser, M. (eds) 2012. Submarine mass movements and their consequences. 5th International Symposium on Advances in Natural and Technological Hazards Research, vol. 31. Dordrecht: Springer, 769 pp.Google Scholar
Yamamoto, Y., Nidaira, M., Ohta, Y. & Ogawa, Y. 2009. Formation of chaotic rock units during primary accretion processes: Examples from the Miura–Boso accretionary complex, central Japan. Island Arc 18, 496–512.Google Scholar
Yamamoto, Y., Ogawa, Y., Uchino, T., Muraoka, S. & Chiba, T. 2007. Large-scale chaotically mixed sedimentary body within the Late Pliocene to Pleistocene Chikura Group, Central Japan. Island Arc 16, 505–7.Google Scholar