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Anna Vozárová, Nickolay Rodionov and Katarína Šarinová

tectonothermal events in Gemericum and adjacent units (Western Carpathians, Slovakia): Contribution by 40 Ar/ 39 Ar dating. Slovak Geol. Mag . 11, 2–3, 155–163. Dickinson W.R. 1970: Interpreting detrital modes of graywacke and arkose. J. Sediment. Petrol. 40, 695–707. Dickinson W.R. & Gehrels G.E. 2003: U–Pb ages of detrital zircon from Permian and Jurassic aeolian sandstones of the Colorado Plateau, USA: paleogeographic implications. Sediment. Geol. 163, 29–66. Dickinson W.R. & Gehrels G.E. 2008: U–Pb ages of detrital zircons in relation to

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Morteza Fattahi, Mariam Heidary and Mohammad Ghasemi

not permit Ghassemi et al . (2014) to use the radiocarbon age of sample Ira.2008/C-IV (1105 ± 30 yr BP) to identify a possible seismic event at the base of unit 27, to be associated with the 958 AD Ray-Taleghan event (M ≈ 7.7). If the MAM age of sample IRA4 (3.5 ± 0.4 ka) has overestimated the true burial age of unit 29, it has positive effect on the interpretation of Ghassemi et al . (2014) to associate trench seismic events to some historical events (e.g., unit 27, to be associated with the 958 AD Ray-Taleghan). Particularly, it may confirms Ghassemi et

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Đurðica Pezelj, Jasenka Sremac and Vladimir Bermanec

(Banovina, Croatia) Geol. Carpath. 62 5 447 461 Hammer O., Harper D.A.T. & Ryan P.D. 2001: PAST: paleontological statistics software package for education and data analysis. Paleont. Electronica 4, 1, 1–9. Hammer O. Harper D.A.T. Ryan P.D. 2001 PAST: paleontological statistics software package for education and data analysis Paleont. Electronica 4 1 1 9 Harzhauser M. & Piller W.E. 2007: Benchmark data of a changing sea — palaeogeography, palaeobiogeography and events in the Central Paratethys during the Miocene

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Anna R Agatova and Roman K Nepop

possible continuation of this channel (lake bay) at the opposite side of the Chagan-Taldura watershed in the main scarp of giant seismically induced landslide in the Taldura river valley. Above the lens there is a thick (about 60–80 m) gravel-dominated section of gray moraine and glacio-fluvial sediments with distinct sandy layers of fluvial origin. The glacial deposits are characterized by a high degree of facies variability, which cause difficulties in distinguishing the different glacial episodes. Before the 2003 Chuya earthquake two clearly distinguished steps were

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Orsolya Sztanó, Michal Kováč, Imre Magyar, Michal Šujan, László Fodor, András Uhrin, Samuel Rybár, Gábor Csillag and Lilla Tőkés

case study from the Danube Basin northern margin (Slovakia). Palaeogeogr. Palaeoclimatol. Palaeoecol. 238, 1-4, 32-52. Kováč M., Andrejeva-Grigorovič A., Baráth I., Beláčková K., Fordinál K., Halásová E., Hók J., Hudáčková N., Chalupová B., Kováčová M., Sliva Ľ. & Šujan M. 2008: Lithology, sedimentology and biostratigraphy of the ŠVM-1 Tajná borehole. Geologické práce, Správy 114, 51-84 (in Slovak with English abstract). Kováč M., Synak R., Fordinál K. & Joniak P. 2010: Dominant events in the northern Danube Basin palaeogeography - a

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Slavomír Nehyba, Jiří Otava, Pavla Tomanová Petrová and Adéla Gazdová

. 2015: The Langhian (Middle Badenian) carbonate production event in the Moravian part of the Carpathian Foredeep (Central Paratethys): a multiproxy record. Facies 61, 1. Hoppe G. 1966: Zirkone aus Granuliten. Berichte der Deutschen Gesellschaft für Geologische Wissenschaften – Reihe B: Mineralogie und Lagerstättenforschung 11, 1, 47–81. Hubert J.F. 1962: A zircon-tourmaline-rutile maturity index and the interdependence of the composition of heavy mineral assemblages with the gross composition and texture of sandstones. J. Sediment. Res . 32, 3, 440

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Michal Kováč, Rastislav Synak, Klement Fordinál, Peter Joniak, Csaba Tóth, Rastislav Vojtko, Alexander Nagy, Ivan Baráth, Juraj Maglay and Jozef Minár

-Carpathian-Pannonian junction area: A case study from the Danube Basin northern margin (Slovakia). Palaeogeogr. Palaeoclimatol. Palaeoecol. 238, 32-52. Kováč M., Andrejeva-Grigorovič A., Baráth I., Beláčková K., Fordinál K., Halásová E., Hók J., Hudáčková N., Chalupová B., Kováčová M., Pipík R., Sliva Ľ. & Šujan M. 2008: Lithology, sedimentology and biostratigraphy of the ŠVM-1 Tajná borehole. Geol. Práce, Spr. 114, 51-84 (in Slovak). Kováč M., Synak R., Fordinál K. & Joniak P. 2010: Dominant events in the northern Danube Basin

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Johann Hohenegger, Stjepan Ćorić and Michael Wagreich

References Abdul Aziz H., Di Stefano A., Foresi L.M., Hilgen F.J., Iaccarino S.M., Kuiper K.F., Lirer F., Salvatorini G. & Turco E. 2008: Integrated stratigraphy and 40Ar/39Ar chronology of early Middle Miocene sediments from DSDP Leg42A, Site 372 (Western Mediterranean). Palaeogeogr. Palaeoclimatol. Palaeoecol. 257, 123-138. Abreu V.S. & Haddad G.A. 1998: Glacioeustatic fluctuations: the mechanism linking stable isotope events and sequence stratigraphy from the Early Oligocene to Middle Miocene. In: Graciansky C.-P., Hardenbol

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Friđgeir Grímsson, Gunver Krarup Pedersen, Guido W. Grimm and Reinhard Zetter

-146. GOLOVNEVA L.B. 2000. Early Palaeogene floras of Spitsbergen and North Atlantic floristic exchange. Acta Univ. Caralinae Geol., 44: 39-50. GOLOVNEVA L.B. & ABRAMOWA L.N. 1990. New plants of the Rarytkin (the Upper Cretaceous, the Koryak upland) [in Russian]. Paleont. Zh., 75: 995-998. GRADSTEIN F.M., OGG J.G., SCHMITZ M. & OGG G. 2012. The Geologic Time Scale 2012. GREGERSEN U., HOPPER J.R. & KNUTZ P.C. 2013. Basin seismic stratigraphy and aspects of prospectivity in the NE Baffin Bay, Northwest Greenland. Mar. Petrol. Geol

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Mateusz Płóciennik, Andrzej Kruk, Danuta J. Michczyńska and John B. Birks

References Abreu CE and de Ribet B, 2002. Trace shape and multi-attribute seismic facies analysis applied to Paleocene/Eocene reservoirs on deep-water Campos Basin. Revista Brasileira de Geofisica 20: 89-95. Agterberg FP and Gradstein FM, 1988. Recent developments in quantitative stratigraphy. Earth-Science Reviews 25: 1-73, DOI 10.1016/0012-8252(88)90099-2. Bedoya D, Novotny V and Manolakos ES, 2009. Instream and off-stream environmental conditions and stream biotic integrity: importance of scale and site