Relevant bibliographies by topics / Kaczawa

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Academic literature on the topic 'Kaczawa'

Author: Grafiati
Published: 4 June 2021
Last updated: 28 July 2025

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Journal articles on the topic "Kaczawa"

1

Malczewski, Dariusz, Martyna Jeleń, Jerzy Żaba, Artur Błachowski, Krzysztof Ruebenbauer, and Maria Dziurowicz. "Identification of iron-bearing minerals in basalts and pillow lavas of the Kaczawa Mountains using 57Fe Mössbauer spectroscopy." Nukleonika 62, no. 2 (2017): 145–48. http://dx.doi.org/10.1515/nuka-2017-0021.

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Abstract The Kaczawa Mountains along with the Kaczawa foothill comprise a complicated geological unit that is called the Kaczawa metamorphic (Sudetes, SW Poland). The aim of our work was to identify the iron-bearing minerals in samples of basalts and pillow lavas from the Kaczawa metamorphic using 57Fe Mössbauer spectroscopy. Based on the preliminary results, the Fe3+/Fe2+ ratio in the samples was determined.
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Golonka, Jan, Maria Barmuta, and Jan Barmuta. "Kaczawa Klippen Belt – geotouristic attraction in the Sudety Mountains, SW Poland." Acta Geoturistica 9, no. 1 (2018): 30–35. http://dx.doi.org/10.1515/agta-2018-0004.

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Abstract In the paper authors present some geological sites from Kaczawa Unit, Sudetes, Poland, and their interpretation in a geotectonic context. All described geosites are important for understanding the evolution of so called Kaczawa Accretionary Prism as well as whole Sudetes. Presented outcrops are easily accessible, well exposed and exhibits high education value. Special attention was given to the Wojcieszów Limestones and their relationship to the surrounding rocks
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3

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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4

Sroga, Cezary, Wojciech Bobiński, and Wiesław Kozdrój. "Geological setting of the barite-fluorite deposit at Jeżów Sudecki (Kaczawa Mts.)." Biuletyn Państwowego Instytutu Geologicznego 472, no. 472 (2018): 231–54. http://dx.doi.org/10.5604/01.3001.0012.7120.

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From 1969 to 1993, investigation for the Ba-F mineralization was executed within the metamorphic Kaczawa complex, north of the Intra-Sudetic Fault in the Jeżów Sudecki-Dziwiszów area (Kaczawa Mts., Western Sudetes). The article presents unpublished results of those prospecting works. A small deposit of Ba-F with Zn, Pb, Cu-sulphides, on the SE slope of the Szybowisko hill near Jelenia Góra, was documented in 1994. The economic mineralization is developed in the Jeżów Sudecki fault, steep fracture zone running parallel to the Intra-Sudetic Fault, and was identified at a distance of 600 m along
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5

Kuchar, Leszek, Ewa Broszkiewicz-Suwaj, Slawomir Iwanski, and Leszek Jelonek. "Comparison of daily flows simulated for the year 2060 on the Kaczawa River for various scenarios of climate change by simple time series analysis." E3S Web of Conferences 100 (2019): 00041. http://dx.doi.org/10.1051/e3sconf/201910000041.

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In this paper a time series analysis for daily flow simulations according three climate change scenario for Kaczawa River a left side tributary of the Odra River in south-west Poland is presented. The flow sequences were simulated using the hydrological model MIKE SHE and the spatial SWGEN meteorological data generator. Meteorological data for the hydrological model were generated based on data from 24 meteorological stations and 35-year daily data from the Institute of Meteorology and Water Management of the National Research Institute (IMGW). Data were generated for future climate condition
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6

Wojewoda, Jurand, Jarosław Wajs, and Dominik Sokalski. "Young geodynamic activity in the marginal fault zone of the Sudetic Block - new data." Geologos 30, no. 2 (2024): 71–80. http://dx.doi.org/10.14746/logos.2024.30.2.08.

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A quarter of a century ago, during cartographic works using then-known field methods for measuring structural features, on the boundary of the Sudetic and Fore-Sudetic blocks, new phenomena were recognised; these were interpreted to be tectonic in nature and the result of left-lateral strike-slip movement in the subsurface. Grabens, half-grabens, shear zones and seismites in the gold-bearing sands and gravels that form the slopes of the valley of the River Kaczawa, are estimated to be of Pliocene and early Pleistocene age, having been interpreted as deposits of the pre-Kaczawa alluvial fan sys
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7

Białek, Dawid, Paweł Raczyński, Przemysław Sztajer, and Dominik Zawadzki. "Archaeocyaths from the Kaczawa complex, West Sudetes, Poland." Journal of Earth Science 21, S1 (2010): 18–20. http://dx.doi.org/10.1007/s12583-010-0159-0.

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8

Wajs, Jaroslaw, Damian Kasza, Paweł P. Zagożdżon, and Katarzyna D. Zagożdżon. "3D modeling of underground objects with the use of SLAM technology on the example of historical mine in Ciechanowice (Ołowiane Range, The Sudetes)." E3S Web of Conferences 29 (2018): 00024. http://dx.doi.org/10.1051/e3sconf/20182900024.

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Terrestrial Laser Scanning is a currently one of the most popular methods for producing representations of 3D objects. This paper presents the potential of applying the mobile laser scanning method to inventory underground objects. The examined location was a historic crystalline limestone mine situated in the vicinity of Ciechanowice village (Kaczawa Mts., SW Poland). The authors present a methodology for performing measurements and for processing the obtained results, whose accuracy is additionally verified.
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9

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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10

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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Books on the topic "Kaczawa"

1

Olczak, Mariusz. Kampania 1813: Slask i Luzyce. Wydawnictwo "Oppidum", 2004.

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2

Cymerman, Zbigniew. Analiza strukturalno-kinematyczna i waryscyjska ewolucja tektoniczna kompleksu kaczawskiego =: Structural and kinematic analysis and the Variscan tectonic evolution of the Kaczawa complex (the Sudetes). Państwowy Instytut Geologiczny, 2002.

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3

Bocheńska, Tatiana. Hydrogeologia zlewni górnej Kaczawy. Wydawn. Uniwersytetu Wrocławskiego, 1994.

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Kostorz, Rudolf. Objazd nad Kaczawą w średniowiecznych dyplomach. Tow. Miłośników Zabrza, 2001.

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5

Brzechwa, Jan. Kaczka-dziwaczka. Podsiedlik Raniowski i spolka, 1993.

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6

Kacziba, Andi. Vìola. Studio Museo Francesco Messina, 2016.

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7

illustrator, Jácome Mauricio, ed. El pato dorado: Zloty kaczka. Ecir Editorial, 2007.

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8

Cymerman, Zbigniew. Strefa kontaktu kaczawskiego kompleksu strukturalnego z depresja ̨Świebodzic (Sudety Środkowe) w świetle nowych otworów badawczych Cieszów PIG 1 i Cieszów PiG 2: The contact zone between the Kaczawa Structural Complex and Świebodzice Depressions (Central Sudetes, SW Poland) in the light of the new research boreholes of Cieszów PIG 1 and Cieszów PIG 2. Państwowy Instytut Geologiczny--Państwowy Instytut Badawczy, 2014.

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9

Molenda, Maria (1978- ) Il, Seweryn Zbigniew Il, Brzechwa Jan (1900-1966), et al., eds. Kaczka dziwaczka: Na straganie ; Samochwała ; Na wyspach Bergamutach. Wydawnictwo Liwona, 2009.

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10

Stolarczyk, Tomasz, and Kamil Nowak. Metalurdzy znad Kaczawy: Cmentarzysko ciałopalne z epoki brązu odkryte w Legnicy przy ul. Spokojnej. Muzeum Miedzi, 2016.

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Book chapters on the topic "Kaczawa"

1

Mikulski, Stanislaw Z., Richard J. Markey, and Holly J. Stein. "Re-Os ages for auriferous sulfides from the gold deposits in the Kaczawa Mountains (SW Poland)." In Mineral Deposit Research: Meeting the Global Challenge. Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_202.

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2

Mikulski, S. Z., S. Speczik, and A. Kozlowski. "Fluid inclusion study of quartz veins from the orogenic Klecza gold deposit in the Kaczawa Mountains (SW Poland)." In Mineral Deposit Research: Meeting the Global Challenge. Springer Berlin Heidelberg, 2005. http://dx.doi.org/10.1007/3-540-27946-6_142.

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Conference papers on the topic "Kaczawa"

1

Jastrzębski, Mirosław, Katarzyna Machowiak, Marek Śliwiński, and Jiří Sláma. "Zircon geochemistry and geochronology of the volcano-sedimentary rocks of the Kaczawa Complex, the Sudetes (SW Poland): new data for early Palaeozoic development of the Saxothuringian basin." In Goldschmidt2023. European Association of Geochemistry, 2023. http://dx.doi.org/10.7185/gold2023.15849.

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2

Tadeusz, Tadeusz. "MEASUREMENT AND ANALYSIS OF A FLOOD WAVE PROPAGATION ON THE KACZA RIVER IN GDYNIA IN NORTHERN POLAND." In 17th International Multidisciplinary Scientific GeoConference SGEM2017. Stef92 Technology, 2017. http://dx.doi.org/10.5593/sgem2017/31/s12.057.

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