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Journal articles on the topic 'Geology – Poland – Tajno Mountains'

Author: Grafiati

Published: 4 June 2021

Last updated: 17 February 2022

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1

Orlowski, Stanislaw. "Cambrian stratigraphy and stage subdivision in the Holy Cross Mountains, Poland." Geological Magazine 129, no. 4 (1992): 471–74. http://dx.doi.org/10.1017/s0016756800019555.

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AbstractThe lithostratigraphic and biostratigraphic subdivisions of the Cambrian sequence in the Holy Cross Mountains of Poland are briefly presented and discussed. In accordance with recent progress in Cambrian stratigraphy and correlation in Great Britain and Scandinavia, a new proposal for chronostratigraphic stages is made. It is suggested that these stages are suitable for the Cambrian areas of central and northwest Europe, comprising Great Britain, Scandinavia and Poland. The formal establishment of the stages, a task for the Commission on Cambrian Stratigraphy, could be made using Briti

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2

Rajchel, Lucyna, and Mariusz Czop. "Hydrogeochemical modelling of chloride mineral water from Rabka spa (Carpathian Mountains, Poland)." Geological Quarterly 56, no. 4 (2012): 681–90. http://dx.doi.org/10.7306/gq.1049.

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3

Żylińska, Anna. "The oldest Cambrian trilobites from the Holy Cross Mountains, Poland: taxonomic, stratigraphic and biogeographic reappraisal." Acta Geologica Polonica 63, no. 1 (2013): 57–87. http://dx.doi.org/10.2478/agp-2013-0002.

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Abstract Żylińska, A. 2013. The oldest Cambrian trilobites from the Holy Cross Mountains, Poland: taxonomic, stratigraphic and biogeographic reappraisal. Acta Geologica Polonica, 63 (1), 57-87. Warszawa. Authorship issues are clarified, new photographic documentation is provided and emended systematic descriptions are presented for the oldest Cambrian trilobite taxa from the Holy Cross Mountains (Poland). Biostratigraphic analysis of the fauna allows correlation with the traditional Holmia kjerulfi-group Zone of Scandinavia, the Callavia Zone of Britain and Newfoundland, the lower and middle p

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4

Gaw?da, A., J. A. Winchester, K. Koz?owski, W. Nar?bski, and J. G. Holland. "Geochemistry and palaeotectonic setting of amphibolites from the Western Tatra Mountains, southern Poland." Geological Journal 35, no. 2 (2000): 69–85. http://dx.doi.org/10.1002/1099-1034(200004/06)35:2<69::aid-gj838>3.0.co;2-v.

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Kozłowski, Rafał, Mirosław Szwed, and Monika Żelezik. "Environmental Aspect of the Cement Manufacturing in the Świętokrzyskie Mountains (Southeastern Poland)." Minerals 11, no. 3 (2021): 277. http://dx.doi.org/10.3390/min11030277.

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The research area located in south-eastern Poland is exposed to alkaline pressure from a cement plant in Nowiny, which has been operating there since 1960. Both biotic and abiotic components of the natural environment remain in the zone of the plant’s negative impact. Their reaction, described according to the concept of geo- and bioindicators, provides valuable information on the state of the natural environment in this area. In 2016–2018, the properties of precipitation were being investigated by determining its pH, EC (specific electrolytic conductivity), and chemical composition in terms o

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6

BREMER, OSKAR, GRZEGORZ NIEDŹWIEDZKI, HENNING BLOM, MAREK DEC, and WOJCIECH KOZŁOWSKI. "Vertebrate microremains from the upper Silurian Winnica Formation of the Holy Cross Mountains, Poland." Geological Magazine 155, no. 7 (2017): 1523–41. http://dx.doi.org/10.1017/s0016756817000681.

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AbstractVertebrate microremains from the upper Silurian Winnica Formation in the Holy Cross Mountains, Poland are described from the Winnica and Rzepin sections. Both sites record the uppermost part of the Słupianka Member, but represent different depositional environments. The Winnica samples come from a low-energy environment, while the Rzepin sample was taken from a high-energy, oolitic facies. Both sites contain thelodontsThelodus parvidens,Thelodus trilobatus, an anaspid cf.Liivilepisand a number of acanthodian scales of ‘nostolepid’, poracanthodid and ‘gomphonchid’ types. Notable differe

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Tokarski, Antek, Ania Świerczewska, Witold Zuchiewicz, Dušan Starek, and László Fodor. "Quaternary exhumation of the Carpathians: a record from the Orava-Nowy Targ Intramontane Basin, Western Carpathians (Poland and Slovakia)." Geologica Carpathica 63, no. 4 (2012): 257–66. http://dx.doi.org/10.2478/v10096-012-0021-7.

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Quaternary exhumation of the Carpathians: a record from the Orava-Nowy Targ Intramontane Basin, Western Carpathians (Poland and Slovakia)The Neogene-Quaternary infill of the Orava-Nowy Targ Intramontane Basin comprises two tiers showing contrasting lithologies. The Neogene tier is largely composed of claystones and siltstones, whereas the Quaternary tier is dominated by gravels. The two sequences are separated by an erosional surface underlain by a regolith. Deposition of the Neogene sequence took place during subsidence of the basin. No prominent relief existed in the area of the present-day

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8

Zapalski, Mikołaj K., and Błażej Berkowski. "The oldest species of ?Yavorskia (Tabulata) from the Upper Famennian of the Holy Cross Mountains (Poland)." Acta Geologica Polonica 62, no. 2 (2012): 197–204. http://dx.doi.org/10.2478/v10263-012-0009-8.

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ABSTRACT Zapalski, M.K. and Berkowski, B. 2012. The oldest species of ?Yavorskia (Tabulata) from the Upper Famennian of the Holy Cross Mountains (Poland). Acta Geologica Polonica, 62 (2), 197-204. Warszawa. A single perfectly preserved colony of a tabulate coral assigned tentatively to the genus Yavorskia Fomitchev, 1931, collected from Upper Famennian beds (Palmatolepis expansa conodont Zone) in a trench located north of the Kowala Quarry (Holy Cross Mts., central Poland) is here described as a new species, ?Y. paszkowskii sp. nov. It differs from other representatives of the genus in the lac

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Botor, Dariusz, Aneta A. Anczkiewicz, István Dunkl, Jan Golonka, Mariusz Paszkowski, and Stanisław Mazur. "Tectonothermal history of the Holy Cross Mountains (Poland) in the light of low-temperature thermochronology." Terra Nova 30, no. 4 (2018): 270–78. http://dx.doi.org/10.1111/ter.12336.

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10

Bröcker, Michael, and Reiner Klemd. "Ultrahigh-Pressure Metamorphism in the Śnieżnik Mountains (Sudetes, Poland): P-T Constraints and Geological Implications." Journal of Geology 104, no. 4 (1996): 417–33. http://dx.doi.org/10.1086/629837.

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11

Steltenpohl, Mark G., Zbignew Cymerman, Erling J. Krogh, and Michael J. Kunk. "Exhumation of eclogitized continental basement during Variscan lithospheric delamination and gravitational collapse, Sudety Mountains, Poland." Geology 21, no. 12 (1993): 1111. http://dx.doi.org/10.1130/0091-7613(1993)021<1111:eoecbd>2.3.co;2.

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12

Nazik, Atike, Șenol Çapkinoğlu, and Emine Șeker. "Famennian ostracods from the Istanbul zone (Gebze, Kocaeli, NW Turkey) and their paleogeographical relations." Geologica Carpathica 63, no. 5 (2012): 355–63. http://dx.doi.org/10.2478/v10096-012-0028-0.

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Abstract Famennian (Late Devonian) ostracods of the Thuringian Mega-Assemblage were recovered for the first time from three incomplete sections of the Ayineburnu Member of the Büyükada Formation in the Denizliköy area (Gebze, NW Turkey), which were sampled for conodonts. Conodont faunas define an interval extending from the Upper rhomboidea? or Lower marginifera Zone into the Middle expansa Zone of the standard Upper Devonian conodont zonation. The ostracod faunas found here consist of species mainly with thin-walls, long spines and often smooth surfaces such as Rectonaria, Tricornina, Orthona

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13

KOSTYLEW, JOANNA, JAN A. ZALASIEWICZ, and RYSZARD KRYZA. "Pervasive near-surface stratal disruption in an accretionary prism setting: Kaczawa Complex, SW Poland." Geological Magazine 154, no. 3 (2016): 651–60. http://dx.doi.org/10.1017/s0016756816000297.

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AbstractThe tectonized and metamorphosed mudrocks within the Variscan accretionary prism of the Kaczawa Mountains in SW Poland comprise sedimentary mélanges together with more coherent stratigraphic units; some represent large olistoliths deposited in a submarine trench. We infer a trend of progressive near-surface stratal disruption in mud-dominated deposits due to dewatering that forms a continuum with subduction-related tectonic structures imposed on unconsolidated sediment during deeper burial. The assemblage of characters suggests that an accretionary prism environment can influence, and

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14

TYSZKA, RAFAŁ, RYSZARD KRYZA, JAN A. ZALASIEWICZ, and ALEXANDER N. LARIONOV. "Multiple Archaean to Early Palaeozoic events of the northern Gondwana margin witnessed by detrital zircons from the Radzimowice Slates, Kaczawa Complex (Central European Variscides)." Geological Magazine 145, no. 1 (2007): 85–93. http://dx.doi.org/10.1017/s0016756807003962.

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AbstractSIMS dating of detrital zircons from the stratigraphically enigmatic Radzimowice Slates of the Kaczawa Mountains (Sudetes, SW Poland), near the eastern termination of the European Variscides, has yielded age populations of: (1) 493–512 Ma, corresponding to late Cambrian to early Ordovician magmatism and constraining a maximum depositional age; (2) between 550 and 650 Ma, reflecting input from diverse Cadomian sources; and (3) older inherited components ranging to c. 3.3 Ga, with age spectra similar to those from Gondwanan North Africa. The new data show that the Radzimowice Slates cann

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15

KRZEMIŃSKA, Ewa, and Leszek Krzemiński. "Magmatic episodes in the Holy Cross Mountains, Poland – a new contribution from multi-age zircon populations." Biuletyn Państwowego Instytutu Geologicznego 474, no. 474 (2019): 43–58. http://dx.doi.org/10.5604/01.3001.0013.0839.

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This contribution reports on new U–Pb zircon age data from magmatic rocks from the Holy Cross Mountains (HCM) of Poland. The analyzed samples were taken from lamprophyre and diabase veins of Podkranów and Janowice-2 as well as from tuff horizon of Kielce Beds (Ludlow). Internal morphologies have been investigated by SEM-BSE and cathodoluminescence images and they have been used as a guide for the selection of genetically various type of grains, e.g. potential auto-, ante- and xenocrysts, that were analyzed by ion microprobe. The U–Pb age of the magmatic events at 414.2 ±6.6 Ma (Kielce tuff), 3

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16

Bednarczyk, Zbigniew. "Evaluating Landslide Remediation Methods Used in the Carpathian Mountains, Poland." Environmental and Engineering Geoscience 25, no. 4 (2019): 272–88. http://dx.doi.org/10.2113/eeg-2158.

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ABSTRACT The aim of this study was to evaluate the results of landslide remediation in the Polish Carpathians. The research for safeguarding the roads and infrastructure was conducted in the years 2005–2018 in nine landslide areas. The interpretation of engineering geology conditions was complex due to the soil-rock nature of the flysch sediment. Movements were activated after heavy rainfalls. In two cases, triggers were connected with the undercutting of the slope or external loading. The research methods included mapping, drilling, index, oedometer, direct shear tests, ground-penetrating rad

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17

Brachaniec, Tomasz, and Anna Wieczorek. "Possible vertebrate coprolites from the Upper Cretaceous (Coniacian) of the Sudetes Mountains (southern Poland)." Carnets de géologie (Notebooks on geology) 16, no. 13 (2016): 349–54. http://dx.doi.org/10.4267/2042/60665.

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18

Radzevičius, Sigitas, Paweł Raczyński, Marius Užomeckas, Audrius Norkus та Andrej Spiridonov. "Graptolite turnover and δ13Corg excursion in the upper Wenlock shales (Silurian) of the Holy Cross Mountains (Poland)". Geologica Carpathica 70, № 3 (2019): 209–21. http://dx.doi.org/10.2478/geoca-2019-0012.

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Abstract The mid–late Homerian Age of the Silurian Period was a time of intense changes in biota, oceanic chemistry, and sea level and is known as the lundgreni extinction (for the graptolite extinctions), the Mulde bioevent (for the conodont turnover event) or the Homerian carbon isotope excursion (CIE) probably related to glacially influenced climate perturbation. New information on this interval from the deep water sedimentary and graptolite succession of the Kielce Region (Holy Cross Mountains, Poland) of the northern margin of the Małopolska Block is presented here based on analysis of th

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19

ŻYLIŃSKA, ANNA, and MONIKA MASIAK. "Cambrian trilobites from Brzechów, Holy Cross Mountains (Poland) and their significance in stratigraphic correlation and biogeographic reconstructions." Geological Magazine 144, no. 4 (2007): 661–86. http://dx.doi.org/10.1017/s0016756807003366.

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A revision of the trilobite fauna from Brzechów in the Holy Cross Mountains (Poland) shows that the assemblage consists of Palaeolenus medius (Bednarczyk), Issafeniella orlowinensis (Samsonowicz), Kingaspidoides sanctacrucensis (Czarnocki), Paradoxides (Acadoparadoxides) oelandicus Sjögren, P. (A.) cf. mureroensis Sdzuy and P. (A.) sp. It is earliest Middle Cambrian in age according to the West Gondwana standard of Geyer & Landing (2004) and can be correlated with the Cephalopyge notabilis Zone of Morocco. Moreover, the co-occurrence of the ranges of P. (A.) oelandicus with P. (A.) cf. mur

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20

Orłowski, Stanisław. "Trilobite trace fossils and their stratigraphical significance in the Cambrian sequence of the Holy Cross Mountains, Poland." Geological Journal 27, no. 1 (1992): 15–34. http://dx.doi.org/10.1002/gj.3350270104.

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21

Studencki, Wieslaw. "Facies and sedimentary environment of the Pinczow limestones (Middle Miocene; Holy cross mountains, central Poland)." Facies 18, no. 1 (1988): 1–25. http://dx.doi.org/10.1007/bf02536793.

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22

KOWALSKI, Aleksander. "LANDSLIDES AND THE INCORRECT INTERPRETATION OF GEOLOGICAL STRUCTURE – EXAMPLES FROM THE SUDETY MOUNTAINS." Biuletyn Państwowego Instytutu Geologicznego 473, no. 473 (2018): 27–48. http://dx.doi.org/10.5604/01.3001.0012.7708.

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Despite the relatively large number of individual landslides recognized and described over the last several years from the Sudety (Sudetes) Mountains (Lower Silesia, SW Poland), most of the papers focused on the geomorphological characterisation of these forms. This paper presents the results of geological and geomorphological mapping of individual landslides, recognized within three geological units: the Wleń Graben (Northsudetic Synclinorium), the Łączna Elevation (Intrasudetic Synclinorium) and the Glinno Graben (Sowie Mountains Block). Particular attention has been paid to the role of the

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23

Rakociński, Michał. "Sclerobionts on upper Famennian cephalopods from the Holy Cross Mountains, Poland." Palaeobiodiversity and Palaeoenvironments 91, no. 1 (2010): 63–73. http://dx.doi.org/10.1007/s12549-010-0045-x.

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24

MARYNOWSKI, LESZEK, PAWEŁ FILIPIAK, and MICHAŁ ZATOŃ. "Geochemical and palynological study of the Upper Famennian Dasberg event horizon from the Holy Cross Mountains (central Poland)." Geological Magazine 147, no. 4 (2010): 527–50. http://dx.doi.org/10.1017/s0016756809990835.

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AbstractIntegrated palynological, organic and inorganic geochemical and petrographical methods have been used for deciphering the depositional redox conditions and character of organic matter of the Famennian Dasberg event horizon from the deep-shelf Kowala succession of the Holy Cross Mountains. The ages of the investigated samples have been established, using miospore data, as VF (Diducites versabilis–Grandispora famenensis) and LV (Retispora lepidophyta–Apiculiretusispora verrucosa) miospore Zones of the Middle/Upper Famennian. In the standard conodont zonation, this corresponds to the uppe

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25

Jonasson, Christer, Marek Kot, and Adam Kotarba. "Lichenometrical Studies and Dating of Debris Flow Deposits in the High Tatra Mountains, Poland." Geografiska Annaler. Series A, Physical Geography 73, no. 3/4 (1991): 141. http://dx.doi.org/10.2307/521019.

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Machowiak, Katarzyna, Andrzej Muszyński, and Richard Armstrong. "High-level volcanic-granodioritic intrusions from Zelezniak Hill (Kaczawa Mountains, Sudetes, SW Poland)." Geological Society, London, Special Publications 234, no. 1 (2004): 67–74. http://dx.doi.org/10.1144/gsl.sp.2004.234.01.06.

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Kuć, Paweł, Piotr Lenik, and Jakub Bazarnik. "Application of the portable spectrometer XRF for the determination of content of some metals in soil: A case study from Holy Cross Mountains (Central Poland)." Biuletyn Państwowego Instytutu Geologicznego 472, no. 472 (2018): 285–302. http://dx.doi.org/10.5604/01.3001.0012.7121.

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The analysis of chemical composition using the portable X-ray fluorescence spectrometer (p-XRF) is recently rapidly developing instrumental research method. This method was applied to analyze the content of selected elements in soil samples from the Strużna region of the Holy Cross Mountains. The Olympus Delta Premium p-XRF spectrometer (4W Ta anode X ray tube, 40 kV, 200 μA current beam, “soil” mode, 135 seconds) was used. Prior to analyze the soil samples, the NIST 2710a and NIST 2711a reference standards were utilized in order to calibrate the p-XRF spectrometer. The maps showing obtained

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Jach, Renata, and Teresa Dudek. "Origin of a Toarcian manganese carbonate/silicate deposit from the Krížna unit, Tatra Mountains, Poland." Chemical Geology 224, no. 1-3 (2005): 136–52. http://dx.doi.org/10.1016/j.chemgeo.2005.07.018.

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29

Narkiewicz, Marek, and Gregory J. Retallack. "Dolomitic paleosols in the lagoonal tetrapod track-bearing succession of the Holy Cross Mountains (Middle Devonian, Poland)." Sedimentary Geology 299 (January 2014): 74–87. http://dx.doi.org/10.1016/j.sedgeo.2013.10.008.

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Gradziński, Ryszard. "Deep blowout depressions in the aeolian Tumlin Sandstone (Lower Triassic) of the Holy Cross Mountains, central Poland." Sedimentary Geology 81, no. 3-4 (1992): 231–42. http://dx.doi.org/10.1016/0037-0738(92)90072-y.

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31

Skompski, Stanislaw, and Michal Szulczewski. "Tide-dominated Middle Devonian sequence from the northern part of the Holy Cross Mountains (Central Poland)." Facies 30, no. 1 (1994): 247–65. http://dx.doi.org/10.1007/bf02536899.

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YANS, J., R. M. CORFIELD, G. RACKI, and A. PREAT. "Evidence for perturbation of the carbon cycle in the Middle Frasnian punctata Zone (Late Devonian)." Geological Magazine 144, no. 2 (2007): 263–70. http://dx.doi.org/10.1017/s0016756806003037.

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New carbon isotopic data from the Devonian of Ardennes (Belgium) and partly from the Holy Cross Mountains (Poland) highlight an abrupt and high-amplitude negative excursion in the punctata conodont Zone. Published information from Moravia and China suggests that this Middle Frasnian negative excursion, jointly with the preceding large-scale positive shift, should be used as a global chemostratigraphic marker. Causation scenarios for this negative ‘punctata Event’ are correlated neither with major biota turnover nor major sea-level changes, but may be related to: (1) the Alamo Impact Event, tha

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Gordon, S. M., D. A. Schneider, M. Manecki, and D. K. Holm. "Exhumation and metamorphism of an ultrahigh-grade terrane: geochronometric investigations of the Sudete Mountains (Bohemia), Poland and Czech Republic." Journal of the Geological Society 162, no. 5 (2005): 841–55. http://dx.doi.org/10.1144/0016-764904-078.

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Krzyszkowski, Dariusz, Anna Krzywicka, Lucyna Wachecka‐Kotkowska, and Waldemar Sroka. "The Middle Pleistocene glaciolacustrine environment of an ice‐dammed mountain valley, Sudeten Mountains, Poland." Boreas 48, no. 4 (2019): 966–87. http://dx.doi.org/10.1111/bor.12396.

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Trela, Wiesław. "Sedimentary and microbial record of the Middle/Late Ordovician phosphogenetic episode in the northern Holy Cross Mountains, Poland." Sedimentary Geology 203, no. 1-2 (2008): 131–42. http://dx.doi.org/10.1016/j.sedgeo.2007.11.006.

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Migaszewski, Zdzisław M., and Agnieszka Gałuszka. "The origin of pyrite mineralization: Implications for Late Cambrian geology of the Holy Cross Mountains (south-central Poland)." Sedimentary Geology 390 (July 2019): 45–61. http://dx.doi.org/10.1016/j.sedgeo.2019.07.004.

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Mustafa, Karwan A., Mark A. Sephton, Jonathan S. Watson, Fivos Spathopoulos, and Piotr Krzywiec. "Organic geochemical characteristics of black shales across the Ordovician–Silurian boundary in the Holy Cross Mountains, central Poland." Marine and Petroleum Geology 66 (September 2015): 1042–55. http://dx.doi.org/10.1016/j.marpetgeo.2015.08.018.

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Smyrnov, I., and N. Levinskova. ""WHITE ELEPHANT" IN UKRAINIAN CARPATHIANS MOUNTAINS: ON RESTORATION OF A FORMER MILITARY ASTRONOMICAL-METEOROLOGICAL OBSERVATORY." Visnyk Taras Shevchenko National University of Kyiv. Military-Special Sciences, no. 2 (39) (2018): 55–58. http://dx.doi.org/10.17721/1728-2217.2018.39.55-58.

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The article deals with the fate of the astronomical-meteorological observatory, which was built in the Eastern Carpathеs on the Hill of Pip-Ivan (height 2028 m) in 1938, when the Carpathian region was part of Poland. Another name of the observatory is "White Elephant", because in the winter under the snow the observatory's house resembles the shape of the elephant. Mount Pip Ivan has a pyramidal shape with the presence of ancient forms of glacial relief, composed of sandstone. The observatory was equipped with the most up-to-date scientific equipment, in particular, a telescope, astrograph and

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Konon, Andrzej. "Successive episodes of normal faulting and fracturing resulting from progressive extension during the uplift of the Holy Cross Mountains, Poland." Journal of Structural Geology 26, no. 3 (2004): 419–33. http://dx.doi.org/10.1016/j.jsg.2003.08.004.

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40

Marynowski, L., M. Narkiewicz, and C. Grelowski. "Biomarkers as environmental indicators in a carbonate complex, example from the Middle to Upper Devonian, Holy Cross Mountains, Poland." Sedimentary Geology 137, no. 3-4 (2000): 187–212. http://dx.doi.org/10.1016/s0037-0738(00)00157-3.

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Strzyżowski, Dariusz, Joanna Fidelus, and Mirosław Żelazny. "Geomorphological changes within a hillslope caused by a windthrow event in the tatra mountains, southern poland." Geografiska Annaler: Series A, Physical Geography 98, no. 4 (2016): 347–60. http://dx.doi.org/10.1111/geoa.12141.

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Migaszewski, Zdzisław, Ewa Starnawska, and Agnieszka Gałuszka. "Gorceixite from the Upper Cambrian Rocks of the podwiśniówka Mine Pit, Holy Cross Mountains (South-Central Poland)." Mineralogia 38, no. 2 (2007): 171–84. http://dx.doi.org/10.2478/v10002-007-0025-6.

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Gorceixite from the Upper Cambrian Rocks of the podwiśniówka Mine Pit, Holy Cross Mountains (South-Central Poland)This report presents the results of a petrographical, mineralogical (SEM/EDS, XRD) and geochemical (XRF, CV-AAS, ICP-MS) study of gorceixite (barium aluminophosphate) from the abandoned Podwiśniówka mine pit. This site is highlighted by the presence of highly acidic pit pond whose chemistry is strongly affected by the exposed pyrite-bearing zone. The gorceixite occurs in the Upper Cambrian carbonaceous clayey shales, quartzites and tuffs in form of minute accumulations varying from

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Chmielowska, D., and B. Woronko. "A source of loess-like deposits and their attendant palaeoenvironment – Orava Basin, Western Carpathian Mountains, S Poland." Aeolian Research 38 (June 2019): 60–76. http://dx.doi.org/10.1016/j.aeolia.2019.04.003.

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Jach, Renata. "Storm-dominated deposition of the Lower Jurassic crinoidal limestones in the Kr�?na unit, Western Tatra Mountains, Poland." Facies 50, no. 3-4 (2004): 561–72. http://dx.doi.org/10.1007/s10347-004-0028-3.

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Jewuła, Karol, Wiesław Trela, and Anna Fijałkowska-Mader. "The Permian–Triassic boundary in continental sedimentary succession at the SE margin of the Central European Basin (Holy Cross Mountains, Poland)." Geological Magazine 157, no. 11 (2020): 1767–80. http://dx.doi.org/10.1017/s0016756820000047.

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AbstractWe studied the upper Permian and Lower Triassic deposits from the northern and northwestern marginal part of the Holy Cross Mountains (SE part of the Central European Basin or CEB, Poland) to examine stratigraphic continuity between these two systems, and to revise the currently existing stratigraphic framework. A previously existing informal lithostratigraphic scheme has been revisited and placed in a broader chronostratigraphic and palaeoenvironmental context. Sedimentary continuity across the Permian–Triassic (P/T) boundary has been confirmed by the presence of Lueckisporites virkki

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TIMMERMANN, H., R. R. PARRISH, S. R. NOBLE, and R. KRYZA. "New U–Pb monazite and zircon data from the Sudetes Mountains in SW Poland: evidence for a single‐cycle Variscan orogeny." Journal of the Geological Society 157, no. 2 (2000): 265–68. http://dx.doi.org/10.1144/jgs.157.2.265.

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Cieszkowski, Marek, Anna Waśkowska, Justyna Kowal-Kasprzyk, et al. "The Upper Cretaceous Ostravice Sandstone in the Polish sector of the Silesian Nappe, Outer Western Carpathians." Geologica Carpathica 67, no. 2 (2016): 149–66. http://dx.doi.org/10.1515/geoca-2016-0010.

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Abstract The Ostravice Sandstone Member was identified and described as a lithostratigraphic unit in the Polish part of the Outer Carpathians. This division occurs in the lowermost part of the Godula Formation, is underlain by variegated deposits of the Mazák Formation or directly by the Barnasiówka and Lhoty formations, and overlain by the Czernichów Member of the Godula Formation. Domination by thick- and very thick-bedded sandstones, conglomeratic sandstones and conglomerates rich in calcareous clasts, mostly of the Štramberk-type limestones, is typical for the Ostravice Sandstone Member. T

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Bednarczyk, Zbigniew. "Identification of flysch landslide triggers using conventional and ‘nearly real-time’ monitoring methods – An example from the Carpathian Mountains, Poland." Engineering Geology 244 (October 2018): 41–56. http://dx.doi.org/10.1016/j.enggeo.2018.07.012.

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Kryza, R., J. A. Zalasiewicz, S. Mazur, P. Aleksandrowski, S. Sergeev, and S. Presnyakov. "Early Palaeozoic initial-rift volcanism in the Central European Variscides (the Kaczawa Mountains, Sudetes, SW Poland): evidence from SIMS dating of zircons." Journal of the Geological Society 164, no. 6 (2007): 1207–15. http://dx.doi.org/10.1144/0016-76492006-137.

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Salamon, Mariusz A., and Michał Zatoń. "A diverse crinoid fauna from the Middle Jurassic (Upper Bajocian–Callovian) of the Polish Jura Chain and Holy Cross Mountains (south-central Poland)." Swiss Journal of Geosciences 100, no. 1 (2007): 153–64. http://dx.doi.org/10.1007/s00015-007-1207-3.

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