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1
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Studia Geologica Polonica
1999 Vol. 115 91-115
EN This paper summarises investigations on radiolarian faunas from the Cretaceous deposits of the Pieniny Succession, Pieniny Klippen Belt, Polish Carpathians. Twenty one species of Radiolaria from the Upper Albian through the Coniacian deposits have been determined. The species determined belong to th[...]
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Studia Geologica Polonica
1999 Vol. 115 75-90
EN The paper presents a list of Cretaceous fossils, mainly bivalves and belemnites, from the Polish and Slovak parts of the Pieniny Klippen Belt, Carpathians. The fossils were collected and determined by Dr L. Horwitz in the years 1924-1939, and revised by Prof. B. Kokoszyńska in 1957. The list of foss[...]
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Studia Geologica Polonica
1999 Vol. 115 117-130
EN Four stages of structural evolution of the Niedzica Castle tectonic window (Pieniny Klippen Belt, West Carpathians, Poland) are distinguished. The first two stages include: (1) the late-Subhercynian (Campanian) nappe folding; and (2) the Laramian (Early Paleocene) refolding of the nappes and their s[...]
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Studia Geologica Polonica
2000 Vol. 117 49-68
EN Based on ammonites Eurystomiceras cf. polyhelictum (Böckh, 1881) and Oppelia flexa (Buckman, 1924), bivalves Camptonectes (Camptonectes) cf. laminatus (Sowerby, 1818) and Bositra buchi (Roemer, 1836), and Laevilamellaptychus, gr. A, cf. ceratoides (Ooster), a Lower Bajocian age (upper part) has been[...]
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Studia Geologica Polonica
2000 Vol. 117 27-35
EN K-Ar dating of a large basalt olistolith, part of the Upper Cretaceous Jarmuta Formation conglomerate, at Biała Woda, Pieniny Klippen Belt (Western Carpathians), yielded two K-Ar ages: 110.6 ą 4.2 Ma and 120.3 ą 4.5 Ma, from columnar-jointed, and platy-jointed parts of the basalt, respectively. The [...]
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Geologia / Akademia Górniczo-Hutnicza im. Stanisława Staszica w Krakowie
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Volumina Jurassica
EN The large quarries at Priborzhavskoye show thick and fairly complete sequences of the Jurassic and Lower Cretaceous deposits representing two different palaeogeographic successions. The bulk of the deposits in the quarries covers a sequence of dark siliciclastic dominated deposits of the Gresten-lik[...]
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Volumina Jurassica
EN Ferromanganese crusts (FMC) and nodules are known from the Jurassic limestones of the Pieniny Klippen Belt (Western Carpathians) as well as in the Alps, the Bethic Cordillera and Sicily, (e.g. Rojkovič et al. 2003, and papers citied therein). FMC and nodules at the Stankowa Skała near Nowy Targ, fir[...]
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Studia Geologica Polonica
2009 Vol. 132 39-69
EN The paper presents selected results of hydrogeological research carried out in the Pieniny National Park and adjacent areas during the period of 1995-2004. The objectives of the studies were to explore the geological environment and conditions of groundwater occurrence, its circulation and drainage [...]
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Studia Geologica Polonica
1998 Vol. 111 155-179
PL Na wzgórzu zamku niedzickiego w Pieninach odsłaniają się trzy skałkowe jednostki tektoniczne obejmujące osady od jury dolnej do kredy górnej włącznie: czorsztyńska, niedzicka i braniska, ponadto formacja jarmucka (najwyższa kreda). Skomplikowana struktura geologiczna wzgórza powstała w wyniku kilkak[...]
EN Three Upper Cretaceous tectonic units built of Lower Jurassic through Upper Cretaceous marine strata (see Birkenmajer, 1963a, 1977, 1986a): the Czorsztyn Unit, the Niedzica Nappe (tectonic scales), and the Branisko Nappe (tectonic scale), and a tectonic scale built of post-nappe conglomerate and fly[...]
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Geological Quarterly
EN The Pieniny Klippen Belt is characterised by diverse lithologies and complex tectonic strukture. The hydrogeological regime of sources can help in the recognition of regional hydrogeological conditions of this lithological-structural unit, as they exemplify groundwaters on the surface in a natural s[...]
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Geology, Geophysics and Environment
EN The purpose of this paper is to identify and characterize a fault zone located within poorly indurated Pliocene clastic strata occurring in the southern part of the Orava Basin on the boundary of Outer and Central Western Carpathians, close to the Pieniny Klippen Belt. The Orava Basin is a part of t[...]
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Studia Geologica Polonica
2000 Vol. 117 7-25
EN Nine sites of the Miocene andesitic intrusions in the Pieniny Mts, Carpathians (Poland), sampled in 1999, were K-Ar dated. The dating was carried out on whole rock, groundmass and monomineral (amphibole) fractions. The present paper completes the K-Ar age study of andesitic intrusions in the Pieniny[...]
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Geology, Geophysics and Environment
EN Refraction surveys were carried out along the border lines between Outer Carpathians, Inner Carpathians and Pieniny Klippen Belt. Measurements were focused on imaging transition zone structured by para-conglomerates, sandstone and clays lenses, crossing in near neighbourhood of Stare Bystre, village[...]
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Annales Societatis Geologorum Poloniae
EN Field and as mineralogical and petrographical examinations of sedimentary rocks present in the area surrounding the Pieniny Klippen Belt were performed. The aim of these investigations was to identify the symptoms of hydrothermal processes within the studied rocks. Moreover, the areas prospective fo[...]
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Volumina Jurassica
EN The ferromanganese crusts (FMC) and nodules at Stankowa Skała near Nowy Targ (Pieniny Klippen Belt, Poland) are developed in pelagic condensed limestones. The crusts appear on an uneven surface of limestones with thinshelled Bositra bivalves dated to the (?)uppermost Bajocian -Callovian. The crusts [...]
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Studia Geologica Polonica
2008 Vol. 131 237-246
EN Geochemical analysis of a basaltic olistolith, K-Ar dated at Lower Cretaceous, which occurs in Upper Cretaceous conglomerates (Jarmuta Formation) of the Pieniny Klippen Belt of Poland, points to trachybasalt field of intraplate basaltoids. The olistolith most probably derived from a volcanic structu[...]
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Studia Geologica Polonica
2008 Vol. 131 269-280
EN The Cenomanian sequence of marls and marly shales interbedded by black shales (Jaworki Formation) from the Niedzica Succession was investigated. These organic carbon-rich horizons may correspond to the event of global anoxity OAE 1d. Major and trace element profiles mirror changing environments of d[...]
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Studia Geologica Polonica
2008 Vol. 131 229-235
EN A new for mal lithos tra tigraphic name, the Szopka Lime stone For ma tion, is in tro duced for fos si lif er ous spotty lime stones (Fleck enkalk fa cies) of Up per Li as sic (Up per Pli ens ba chian = Domerian) age, de vel oped in pe lagic basi nal suc ces sions of the Pi en iny Klip pen Belt of P[...]
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Geological Quarterly
EN Middle and Upper Juras siclime stones from the Polish part of the Pieniny Klippen Belt (PKB) were palaeomagnetically studied at six localities. The Middle Jurassic redcrinoidal lime stones of the Krupianka Lime stone Formation and Oxfordian radiolarites of the Czajakowa Radiolarite Formation, samp[...]
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