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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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Volumina Jurassica
EN The Late Jurassic source rock studies included thirty six hydrocarbon provinces worldwide. Regions were evaluated to obtain the Source Rocks Prediction Value (SRPV). The effectiveness of three major processes (biologic productivity, depositional preservation, and non-dilution) responsible for organi[...]
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Volumina Jurassica
EN Today the Ukrainian Mesozoic volcanic rocks are located in the relatively small area. They are concentrated near the Rachiv Massif and Chivchin Ridge, generally in the front of the Rahiv and Maramuresh (=Marmaros) nappes (Outer Flysch Carpathians) and in the Pieniny Klippen Belt. Several outcrops in[...]
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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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Prace Instytutu Nafty i Gazu
2006 nr 137 247-253
PL Metoda inwersji sejsmicznej rozwija się począwszy od końca lat 70. ubiegłego wieku. Ostatnie jej modyfikacje to Impedancja Elastyczna, Metoda Lambda-Mu-Rho oraz Inwersja Symultaniczna. Metody te bazują na danych sejsmicznych przed sumowaniem. Łączą metodę inwersji na sumie oraz metodę AVO (Amplitude[...]
EN Acoustic impedance method has been developing since the end of 1970 years. The currently modifications of inversion methods are Elastic Impedance, Lambda-Mu-Rho and Simultaneous Inversion. All of these last methods based on the prestack seismic data and combined typical postack inversion with AVO me[...]
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Prace Instytutu Nafty i Gazu
2006 nr 137 231-239
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Przegląd Geologiczny
2001 Vol. 49 nr 9 785-792
PL Wypełnienie żył w obrębie jednostek tektonicznych Karpat w południowo-wschodniej części obszaru Polski stanowią kwarc, kalcyt i bituminy. Kwarc ma charakter "diamentów marmaroskich". Zawiera szereg inkluzji fluidalnychwęglowodorowych (o składzie od metanu po lekkie ropy) i roztworów wodnych. Charakt[...]
EN Quartz, calcite and bitumens occur in veins within the Carpathian tectonic units in the south easternmost part of Poland. Quartz has a character of the ,,Marmarosh diamonds ". This contains various fluid inclusions of hydrocarbon type (from methane to light oils) and aqueous type. The delta^18 OSMOW[...]
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Biuletyn Państwowego Instytutu Geologicznego
2001 nr 396 122-123
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Biuletyn Państwowego Instytutu Geologicznego
2001 nr 396 113-115
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Biuletyn Państwowego Instytutu Geologicznego
2001 nr 396 52-53
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Biuletyn Państwowego Instytutu Geologicznego
2001 nr 396 123-124
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Acta Geophysica
EN This publication is a contribution to discussion on the geometry and petrography of the rock complex responsible for the Carpathian conductivity anomaly. We analysed arguments showing that this anomaly is caused by induction in the sedimentary basin, and make a critical review of various data to fin[...]
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Biuletyn Państwowego Instytutu Geologicznego
2001 nr 396 118-118
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Biuletyn Państwowego Instytutu Geologicznego
2001 nr 396 139-140
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Biuletyn Państwowego Instytutu Geologicznego
2001 nr 396 81-81
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Biuletyn Państwowego Instytutu Geologicznego
2001 nr 396 45-46
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