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1
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Studia Geologica Polonica
1999 Vol. 114 7-33
EN The age of some Lower Cretaceous lithostratigraphic units and their boundaries in the Guaniguanico terrane, western Cuba, is modified on the basis of calpionellids, foraminifers and nannoconids. In the Northern Rosario belt, the Artemisa/Polier formations boundary is diachronous (upper Lower Berrias[...]
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Studia Geologica Polonica
2003 Vol. 121 81-158
EN The paper presents facies development and lithostratigraphy of the mid-Cretaceous Zabijak Formation in the Polish part of the Tatra Mountains. Reference is also made to all known occurrences of the formation in the Slovak part of the Tatra. Geological maps, general and detailed sections, and represe[...]
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80%
Biuletyn Państwowego Instytutu Geologicznego
2001 nr 396 106-107
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Bulletin of the Polish Academy of Sciences. Earth Sciences
EN Caledonian basement (Hecla Hoek Succession) of the Carboniferous through Tertiary platform coyer is exposed at Midterhuken, Bellsund, Spitsbergen. It consists of three rock-units, so far attributed to the "Magnethogda sequence" believed to represent Middle Proterozoic. In the present author's opinio[...]
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Studia Geologica Polonica
2001 Vol. 118 5-188
EN The paper is an annotated illustrated lexicon of the Mesozoic and Cenozoic stratigraphic units currently in use in the South Shetland Islands and the Northern Antarctic Peninsula (West Antarctica). Formal and informal lithostratigraphic, biostratigraphic and climatostratigraphic units of various ran[...]
6
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Geological Quarterly
EN In the Nowy Sacz Basin, newly exposed Middle Miocene deposits have been studied and sampled in the Kamienica Nawojowska, Poprad and Dunajec rivers. The calareous nannoplankton of the freshwater to marine deposits was examined. Palegrey and brown clayey shales with plant remains and thin seams of [...]
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Geology, Geophysics and Environment
2016 Vol. 42, no. 1 142--143
EN Prins Karls Foreland (PKF) is a westernmost island of Svalbard Archipelago belonging to the Southwestern Basement Province. The island consists of low-metamorphic facies probably Neoproterozoic metasediments, divided into two, northern and southern parts. Both parts are characterized by similar geol[...]
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Studia Geologica Polonica
2003 Vol. 121 7-50
EN The Kościeliska Marl Formation (Middle-Upper Berriasian to Lower Aptian) terminates the Lower Subtatric Succession in the Western Tatra Mountains. The Upper Berriasian to lowermost Hauterivian deposits of the lower part of this formation are subdivided into four members (Pod Furkaską Member, Kryta M[...]
9
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Geological Quarterly
2004 Vol. 48, No 4 351--370
EN The region between the Wieliczka Foothills and the Beskid Makowski Mts. has yielded new data on the accumulation of loess-like deposits during the Vistulian Glaciation. The grain-size distibution and the heavy mineral composition, particularly the significant presence of amphiboles, indicates on aeo[...]
10
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Annales Societatis Geologorum Poloniae
EN This paper deals with the lithostratigraphic correlation of the Ordovician-Silurian succession between the Baltic, Podlasie and Lublin basins, located on the SW slope of the East European Craton. The correlation is based on previous lithostratigraphic classifications, which are modified here to incl[...]
11
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Geology, Geophysics and Environment
2019 Vol. 45, no. 4 305--318
EN The Tsodilo Hills Group strata exposed in the Tsodilo Hills are an association of meta-arenites, metaconglomerates, quartz-mica schists, sandstone, red siltstone and sedimentary breccia deposited on an open siliciclastic marine shelf between the Late Palaeoproterozic and Late Mesoproterozoic, and ou[...]
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Geological Quarterly
EN Multiproxy data (plant macrofossils, AMS 14C radiocarbon dates, grain-size distribution, loss-on-ignition and magnetic susceptibility) from Lake Udriku Suurjärv in North Estonia were used to interpret local environmental changes during the postglacial period between 13 800 and 11 000 cal [...]
13
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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[...]
14
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Geological Quarterly
EN The Paleogene deposits of central-western Poland area have been studied in more than 300 bore holes and several out crops with lithological, mineralogical and sedimentological methods. Grain-size analyses, heavy mineral analyses, XRD analyses and pebble analyses were mainly used to characterize thes[...]
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Bulletin of the Polish Academy of Sciences. Earth Sciences
EN Martinfjella, a submeridional mountain chain which divides the glaciers Antoniabreen from Recherchebreen, NW Torell Land, Spitsbergen, was so-far believed to consist of Middle Proterozoic rocks attributed to the "Magnethogda sequence". In the present author's opinion, this sequence consists of rock-[...]
16
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Bulletin of the Polish Academy of Sciences. Earth Sciences
EN The present paper deals with the Upper Paleocene - Lower and Middle Eocene deposits in the Siary Subunit of the Magura Nappe in the area of Sucha Beskidzka, Polish Outer Carpathians. They are represented by variegated shales of the Łabowa Shale Formation intercalated with thick-bedded sandstones tra[...]
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Geological Quarterly
2005 Vol. 49, No. 4 379--402
EN This paper provides the results of a new litho- and biostratigraphic study from the contact zone between the Magura Nappe and Pieniny Klippen Belt close to Polish-Slovakian border. In the southernmost part of the Krynica facies zone of the Magura Nappe two new lithostratigraphic units have been esta[...]
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Geochronometria
2000 Vol. 18 35-40
EN On the basis of lithostratigraphic analysis of deposits forming the Wolin End Moraine as well as radiocarbon dating of the intercalations of organic matter found amongst such deposits, the age of glaciotectonic structures existing in the area of morainic hills was determined. It is claimed that both[...]
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Geological Quarterly
2012 Vol. 56, No. 4 821--832
EN Eocene thin-bedded flysch, widespread in the Alpine Tethys ocean, is present within the Magura Nappe, the largest Outer Carpathian unit in Poland and Slovakia. Thin-bedded flysch sedimentation accompanied by hemipelagic shales took place accross the entire Magura Basin during Eocene times. The litho[...]
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Przegląd Geologiczny
EN The study of the Ordovician conducted in the Holy Cross Mts. during the last two decades provided new data concerning lithology and stratigraphy of this system. Thus, the revised Ordovician lithostratigaphy of the Holy Cross Mts., presenting a complex temporal stratigraphic and lithofacies pattern i[...]
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