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Tytuł:
Chemiczne frakcjonowanie cynku w osadach rzecznych dorzecza południowej i środkowej Wisły
Chemical fractionation of zinc in bottom sediments of the southern and middle Vistula River drainage basin
Autorzy:
Świetlik, R.
Rabajczyk, A.
Trojanowska, M.
Powiązania:
https://bibliotekanauki.pl/articles/2074652.pdf
Data publikacji:
2009
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
cynk
frakcjonowanie
osaday rzeczne
zinc
fractionation
river sediments
Opis:
In Poland, the average Zn contents in river sediments keep up the level 100 mg/kg. The largest accumulations of zinc (up to 10 000 mg/kg), found in river sediments in the Upper and Lower Silesia area, are the result of mining and industrial activity in these regions. In the remaining parts of the country the contents are clearly smaller, except for the conurbation areas (Lis & Pasieczna, 1995). At present, forecasts of behavior of me- tals present in solid environmental samples are usually based on results of chemical fractionation. In this approach, metals are extracted by treating samples with solutions of increasing solubilization potential and simulating extgraction of metals under natural and anthropogenically modified environmental conditions (Rauret, 1998). The studies covered speciation of zinc in river sediments of the Nida and Radomka drainage basins. The chemical fractionation of zinc was conducted in accordance with three-stage procedure of sequential extraction BCR (at present, Standard Measurement and Testing Program), worked out by Ure et al. (1993). The aim of investigations was to compare forms of occurrence of zinc in sediments of rivers flowing through areas differing in geochemical background and characterized by differences in content of anthropogenic zinc. The speciation of zinc in sediment samples from the Radomka drainage basin gave results clearly different from those for sediments from the Nida drainage basin, which may reflect differences in land use. The content of zinc in the studied samples was found to change for 8 mg/kg in bottom deposits of Radomka River at Domaniów to 267 mg/kg in those of Mleczna River at Firlej in the Radomka drainage basin and from 88 mg/kg in sediments of Maskalis River at Brzezie to 101 mg/kg in those of the Brzeźnica River at Raków in the Nida drainage basin.
Źródło:
Przegląd Geologiczny; 2009, 57, 12; 1101-1105
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Charakterystyka osadów facji powodziowej współcześnie deponowanych w dolinie rzeki Dunajec i w Jeziorze Rożnowskim (południowa Polska)
Characteristics of flood sediments recently deposited in the Dunajec River valley and Rożnowskie Lake
Autorzy:
Gwóźdź, R.
Powiązania:
https://bibliotekanauki.pl/articles/2075469.pdf
Data publikacji:
2016
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
mady
osady powodziowe
osady rzeczne
analiza fizyczna gleby
Jezioro Rożnowskie
alluvial soils
flood sediments
river sediments
physical analysis of soil
Rożnowskie Lake
Opis:
The paper presents the results of geotechnical properties of cohesive soil recently deposited in Rożnowskie Lake and on the floodplain of the Dunajec River. The results show that cohesive soils of Rożnowskie Lake are represented mainly by silt, clay and silty clay. Sandy silt and silt are deposited predominantly on the floodplain of the Dunajec River. The soils contain a few percent of organic matter, however, there is more organic matter in the sediments of Rożnowskie Lake. The variability of deposited soils is due to different periods of sedimentation on an annual basis. The time of sedimentation on the Dunajec River floodplain is short and associated with flooding during the summer culmination, thus the sediments (sandy silt and silt) are coarsest. In the area of Rożnowskie Lake, sludge sedimentation occurs throughout the year, especially during the spring and summer flood flow. This sludge has finer grain size (silt and clay). The soils show a variation in their vertical profile, and are characterized by a layered structure.
Źródło:
Przegląd Geologiczny; 2016, 64, 10; 799--805
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Pobór i opróbowanie powierzchniowych, silnie uwodnionych osadów jeziornych o nienaruszonej strukturze-uwagi metodyczne i stosowany sprzęt
Coring and subsampling of undisturbed recent lake sediments with high water content-remarks about methodology and equipment
Autorzy:
Tylman, W.
Powiązania:
https://bibliotekanauki.pl/articles/2074556.pdf
Data publikacji:
2007
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
osady jeziorne
pobór
próbnik grawitacyjny
lake sediments
coring
gravity corer
core sectioning
Opis:
This study presents some remarks about coring and sectioning cores of recent lake sediments. Effective coring of such sediments is not easy because they are very loose (water content usually exceeds 90%]. Precisely taken core should consist of near-bottom water and undisturbed sediment column. The most widely used are gravity corers which are simple in construction and operation. The gravity corer presented here is additionally equipped with percussion system to improve penetration into the sediment. It enables to take cores 94 mm in diameter and up to 90 cm in length. The corer with rubber stopper blocked is lowered through the water and pushed into the sediment. While retrieving the core, the stopper settles into the top of the core tube. At the surface, the plug is inserted into the bottom of the core tube. After collecting, the core should be extruded and sectioned. A device presented here enables to divide the core into short intervals [0.5-1 cm]. The core is extruded upwards and samples can be collected from the tray placed on top of the tube. Both the corer and the extruder are relatively small and light. This equipment have been used in the Department of Geomorphology & Quaternary Geology at Gdańsk University for several years. So far, cores from more than 60 lakes of various depths [up to 50 m] have been successfully taken.
Źródło:
Przegląd Geologiczny; 2007, 55, 2; 151-156
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wpływ budowy geologicznej i ukształtowania terenu na historyczne i współczesne inwestycje inżynierskie i budowlane w Lublinie
Impact of geology and relief on the historical and contemporary on the engineering and construction investments in Lublin
Autorzy:
Mroczek, P.
Powiązania:
https://bibliotekanauki.pl/articles/2074274.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Lublin
Wyżyna Lubelska
less
osady powierzchniowe
inżynieria
Lublin Upland
loess
surface sediments
engineering
Opis:
The first geological and engineering investments in Lublin related to the defense and the isolation of the castle can be dated back at least 700 years. Today, the oldest ones among them are documented only during archaeological excavations in the areas of hills/promontories in the eastern edge of loessic Na³êczów Plateau, steeply sloping down to the valley of Bystrzyca River. Over the centuries, the growing town, required number of investments conditioned by the geology (surface rocks) and relief. The city expanded to the areas of different in geology and topography. As a result of geotechnical works, implemented over several hundred years, modern Lublin is the town that could boast a number of multiage and diverse geotechnical objects. These are primarily objects designed to serve the defense, streamlining communication and also widely understood economy.
Źródło:
Przegląd Geologiczny; 2014, 62, 10/2; 645--653
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Chloroorganiczne pestycydy i polichlorowane bifenyle w osadach rzek Polski
Chlorinated pesticides and polychlorinated biphenyls in river sediments of Poland
Autorzy:
Bojakowska, I.
Gliwicz, T.
Powiązania:
https://bibliotekanauki.pl/articles/2074353.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
związki chloroorganiczne
zanieczyszczenia
osad rzeczny
geochemia osadów
chlorinated compounds
pollution
river sediments
Polska
Opis:
Concentrations of chlorinated pesticides and polychlorinated biphenyls (PCB28, PCB52, PCB101, PCB118, PCB153, PCB138, PCB180), were determined in 80 river sediment samples collected from the whole area of Poland. Chlorinated pesticides were found in almost all samples. The most frequently detected pesticides were isomer y-HCH (Lindane) and the DDT group compounds. The concentrations of Lindane exceeding the detection limit were recorded in 95% of samples and Lindane contents above the PEL value were noted in 32.5% of the analysed samples. The high contests of pesticides were recorded mainly in river sediments near urban-industrial centres. The presence of p,p’-DDT was noted in 31 samples and its metabolite p,p’-DDE —in 78 samples, and p,p’-DDD —in 69 samples. The concentration of p,p’-DDE above PEL value (6.75 ug/kg) were detected in 9 samples, p’-DDD (8.51 ug/kg) —in 9 samples, p,p’-DDT —in 13 samples. Of the remaining pesticides the concentrations of heptachlor epoxide exceeding the detection limit were observed in 5 sediment samples, Dieldrin —in 15 samples, Aldrin —in 10 samples, Endrin —in 10 samples, Endosulfan I only in 1 sample, Endosulfan II — in 4 samples and Methoxychlor — in 2 samples. The concentrations of Heptachlor epoxide higher than the PEL value (2,74 ug/kg) were detected in 1 sample (1.3%). Of 48.8% of the analysed river sediment samples contained polychlorinated biphenyls above detection limit; in two locations the PCB concentrations were high enough to pose a threat for water organisms.
Źródło:
Przegląd Geologiczny; 2005, 53, 8; 649--655
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Minerały autigeniczne i osady w strefie hyporeicznej aluwiów Białej Przemszy zanieczyszczonej przez górnictwo rud metali
Authigenic minerals and sediments in the hyporheic zone of the Biała Przemsza River polluted by metal ore mining
Autorzy:
Ciszewski, D.
Kucha, H.
Skwarczek, M.
Powiązania:
https://bibliotekanauki.pl/articles/2075696.pdf
Data publikacji:
2017
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
osady rzeczne
skażenie
mineralogia
strefa hyperheiczna
Biała Przemsza
river sediments
pollution
mineralogy
hyporheic zone
Opis:
Sediments and waters of the hyporheic zone have been investigated in the middle reach of the Biala Przemsza River (southern Poland). The river is polluted with mine waters dischargedfrom lead-zinc ore mines, and ground waters sampled from piezometers in a sand bar are polluted to a similar degree down to a depth of at least 3 m. Very high content of heavy metals in the upper 1 m-thick strata of the bar indicates that their accumulation follows start-up of the lead-zinc mining in the mid-20th century. Common authigenic pyrite, gypsum and other less widespread heavy metal minerals are observed in the sediments of both the mining- and pre-mining times. It is related to the intense infiltration of sulphate-rich waters into the sand bar and microbially controlled anoxic conditions, which favour pyrite formation.
Źródło:
Przegląd Geologiczny; 2017, 65, 10/1; 650--660
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Nowe stanowiska laminowanych osadów jeziornych na Pojezierzu Kaszubskim
New sites of laminated lake sediments in Kashubian Lakeland
Autorzy:
Tylmann, W.
Zawadzka, M.
Powiązania:
https://bibliotekanauki.pl/articles/2074616.pdf
Data publikacji:
2008
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
stanowiska laminowanych osadów jeziornych
roczna laminacja
Pojezierze Kaszubskie
laminated lake sediments
annual lamination
Kashubian Lakeland
Opis:
Annually laminated lake sediments are a very valuable source of paleoecological information because they provide a precise timescale in calendar years and limited post-depositional disturbances. They are formed in specific conditions that enable not only the formation but also preservation of lamination, hence they rarely occur. The goal was to find lakes with annually laminated sediments in Kashubian Lakeland which can provide new high-resolution paleoenvironmental and paleoclimatic data for this part of Europe. Based on statistical analyses including catchment geology and topography, morphometric lake basin features and hydrological parameters, a pre-selection of 22 lakes with water depths ranging from 15 to 35 m was carried out. Gravity cores (30–90 cm long) were obtained from 18 of these lakes during a field survey in 2006. The cores were split lengthwise, photographed digitally and examined carefully. Four of the lakes studied show distinct alternations of pale and dark laminae. For three lakes (Kramsko Duże, Kramsko Małe and BorowoWielkie) such laminations were restricted to sections of the cores only. Lake Suminko was deemed the most promising site with its laminations covering the entire taken core. In all the cases, biochemical varves were developed with pale spring/summer layers composed of autochthonous carbonates and dark fall/winter layers made of organic detritus and minerogenic particles.
Źródło:
Przegląd Geologiczny; 2008, 56, 5; 404-408
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Akumulacja osadów na równinach zalewowych rzek silnie zmienionych antropogenicznie: górna Wisła i Odra
Sediment accumulation on alluvial plains of the heavily impacted river reaches: upper Vistula and Odra, southern Poland
Autorzy:
Ciszewski, D.
Czajka, J.
Powiązania:
https://bibliotekanauki.pl/articles/2074705.pdf
Data publikacji:
2009
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
osady rzeczne
akumulacja
zmiany koryta
skażenie
metale ciężkie
river sediments
accumulation
channelization
pollution
heavy metals
Opis:
Overbank sediment profiles of the channelized and heavily polluted Vistula and Odra rivers were investigated in southern Poland. The sediments are usually represented by sandy layers about a dozen centimetres thick, intercalated with black sandy muds few centimetres thick and rich in organic matter. Accumulation of these sediments started by the end of 19th century. The sediments are contaminated with heavy metals in amounts exceeding background values by two orders of magnitude and contain coal particles dispersed in black layers. These fine sediments initially accumulated over gravel bars at the channel banks due to lateral channel stabilization by stony groynes and bank revetments, constructed in 19th and 20th century. Progressively the sediments, which are up to 4 m thick, became a part of 20–30 m wide floodplain zones along many reaches of the upper Vistula and Odra. The distribution of these sediments is related to the degree of channel narrowing and incision induced by 19th and 20th century channelization.
Źródło:
Przegląd Geologiczny; 2009, 57, 7; 576-576
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Osady biogeniczne interglacjału eemskiego w Porzewnicy i Marysinie koło Mińska Mazowieckiego (Obniżenie Węgrowskie)
Biogenic deposites of the Eemian Interglacial at Porzewnica and Marysin near Minsk Mazowiecki (Wegrów Basin-Central Poland)
Autorzy:
Bruj, M.
Krupiński, K.M.
Powiązania:
https://bibliotekanauki.pl/articles/2074476.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
intergracjał eemski
osad biogeniczny
stratygrafia
Eemian Interglacial
Węgrów Basin
lacustrine sediments
pollen analysis
stratigraphy
palynostratigraphy
Opis:
Ice sheet of the Wartanian Glaciation and their deposits shaped the landscape of the Węgrów Basin. Biogenic lake sediments at Porzewnica and Marysin sites (figs.1, 2) consist of about 5 m thick silts and gyttja, covered by 1.15 m thick sand at Porzewnica and by 8.5 m thick silts and sands at Marysin. In the Porzewnica pollen diagram (fig. 4) there are 7 L PAZ and 1 interzone without sporomorphs. representing vegetation succession during the late Wartanian Glaciation, the protocratic, mesocratic and part of the telocratic phases of the Eemian Interglacial. Spectra of sediments at the Marysin site represent 4 L PAZ of the youngest part of the mesocratic phase and fragments of the telocratic phase of that Interglacial.
Źródło:
Przegląd Geologiczny; 2006, 54, 2; 154--160
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Miedź, nikiel, ołów i cynk w strefach wpływu eksploatacji złóż miedzi Dolnego Śląska
Copper, nickel, lead and zinc in the zones affected by exploitation of copper deposits in the Lower Silesia
Autorzy:
Duczmal-Czernikiewicz, Agata
Hoska, Natalia
Zimny, Marcin
Zimny, Daniel
Powiązania:
https://bibliotekanauki.pl/articles/2075969.pdf
Data publikacji:
2019
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
miedź
nikiel
ołów
cynk
gleby
osady
Dolny Śląsk
copper
nickel
zinc
lead
soils
sediments
Lower Silesia
Opis:
Base metals (Cu, Zn and Pb) as the main resources of the Lower Silesian copper deposits have significantly been influenced by different enviromentalfactors. In this paper, changes in metal concentrations on the surface in relation to deeper layers of the sediments were examined. The concentration ofmetals in the whole sediment, and in selected grain fractions was studied. The contents of these metals in the soils of areas adjacent to the deposit are diverse and are in the range of: 3.0-1082.9 mg/kg Cu; 3.5-106.1 mg/kg Pb; 27.6-49.3 mg/kg Zn, and 1.33-23.0 mg/kg Ni in the old deposit district and Cu 0.91-1655.0 mg/kg Pb; 10.0-1792.0 mg/kg Zn; 3.38-1129.0 and 0.47-32.7 mg/kg Ni in the new deposit district. The increase of metal concentration in the finefractions has been observed. Moreover, the decrease in the metal content with depth was observed in all investigated profiles.
Źródło:
Przegląd Geologiczny; 2019, 67; 154--155
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Kartograficzne badania geochemiczne w Polsce
Geochemical Mapping in Poland
Autorzy:
Pasieczna, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075819.pdf
Data publikacji:
2018
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
mapy geochemiczne
badania podstawowe
gleby
osady
woda
Polska
geochemical maps
baseline studies
soils
sediments
water
Polska
Opis:
At the beginning of the 1990s, both in Poland and in the world, the field of applied geochemistry was extended to issues related to the protection of the Earth’s natural environment due to the growing social interest in this problem and the requirements of the existing legislation. Geochemical studies in Poland were carried out in three stages, proceeding from the review scale (1:500,000 -1 stage) through regional research (on a scale from 1:250,000to 1:50,000 -stage II) to detailed research (on a scale of1:25,000 to 1:10,000 -stage III). The first stage of the geochemical mapping allowed for quick and relatively inexpensive assessment of the geochemical background diversity of soils, sediments, and surface water throughout the country, as well as the indication of the most polluted regions. The regional research (II stage) was focused primarily on issues related to the explanation of the origin of the identified geochemical anomalies detected in the first stage of research. They were taken in selected urban-industrial areas. In the most polluted Silesian-Cracow region a detailed geochemical study is being carried out (III stage).
Źródło:
Przegląd Geologiczny; 2018, 66, 6; 344--352
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Zawartość metali ciężkich (Cu, Zn, Pb, w wybranych elementach ekosystemu estuarium Odry Co, Cd, Hg)
The contents of heavy metals (Cu, Zn, Pb, Co, Cd, Hg) accumulated in selected components of the Odra River Estuary ecosystem
Autorzy:
Piotrowski, S.
Powiązania:
https://bibliotekanauki.pl/articles/2074530.pdf
Data publikacji:
2007
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
metale ciężkie
osady denne
mięczaki
ujście rzeki Odry
heavy metals
bottom sediments
molluscs
Odra River estuary
Opis:
The content of Cu, Zn, Pb, Co, Cd and Hg accumulated in water, mollusc shells and 15-cm layer of bottom sediments in Lake D1bie, Domi1?a and Roztoka Odrzanska is analysed. The metal concentrations range from 99.82 to 99.88% in bottom sediments, from 0.09 to 0.16% in water and from 0.01 to 0.04% in shells. There is some diversity in distribution of heavy metals in bottom sediments of the study areas due to diversity of heavy metal concentrations in the Odra River Estuary. The metal successions in mollusc shells of the three areas under consideration are identical: Zn > Cu > Pb > Cd > Hg. The distribution of metals in water and mollusc shells indicates greater concentrations of metals in molluscs. In particular, when considering the mass ratio, the water mass is greater than the mass of shells, varying from 3100 (Lake Dąbie) to 20000 (Domiąża). The content of metals in the shells ranges from 7.33% to 22.39% of their total amount in the analysed ecosystems.
Źródło:
Przegląd Geologiczny; 2007, 55, 6; 213-218
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Geochemiczny zapis diagenezy szczątków kostnych z Jaskini Deszczowej (Wyżyna Częstochowska)
Geochemical record of diagenesis of bone remains fromDeszczowa Cave (Częstochowa Upland)
Autorzy:
Krajcarz, M.
Powiązania:
https://bibliotekanauki.pl/articles/2066279.pdf
Data publikacji:
2010
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
diageneza szczątków kostnych
osady jaskiniowe
czwartorzęd
Polska
Deszczowa Jaskinia
bone diagenesis
cave sediments
Quaternary
Polska
Deszczowa Cave
Źródło:
Przegląd Geologiczny; 2010, 58, 2; 163-172
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wykorzystanie 210Pb i metali ciężkich do oceny tempa współczesnej sedymentacji zanieczyszczonych osadów fluwialnych w dolinie górnej Warty
Using 210Pb end heavy metals to estimate Recent sedimentation rates of polluted fluvial deposits in Upper Warta River Valley
Autorzy:
Łokas, E.
Ciszewski, D.
Wachniew, P.
Owczarek, P.
Powiązania:
https://bibliotekanauki.pl/articles/2074425.pdf
Data publikacji:
2006
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
210Pb
depozycja
osad fluwialny
metale ciężkie
historia zanieczyszczenia środowiska
river sediments
sedimentation rate
heavy metal
pollution history
Opis:
River floodplains have been recognized as an important sink for suspended sediments and associated contaminants mobilized from upstream catchments. However, information on rates of overbank sedimentation within time span of several tens of years is impossible to obtain using conventional sediment traps. Measurements of the 210Pb content in floodplain sediments provide an alternative approach for obtaining estimates of medium-term (100–150 years) rates of overbank sediment deposition. The use of 210Pb method and heavy metals concentration profiles allowed to obtain retrospective estimates of recent sedimentation rates on floodplain of the Warta River (the Cracow Upland, southern Poland). The results are compared with dating of sediment layers by characteristic peaks of heavy metal concentrations. The highest sediment accretion rate, of the order of 1 cm/year, was found in a levee along river bank. Sediment deposition in flood basin is much slower and usually does not exceed 1 mm/year.
Źródło:
Przegląd Geologiczny; 2006, 54, 10; 888-894
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rozwój rynny Miazgi–Wolbórki (Polska środkowa) w świetle analizy jej wypełnienia
Formation of the Miazga-Wolbórka tunnel valley (central Poland) based on an analysis of its infill
Autorzy:
Rdzany, Zbigniew
Frydrych, Małgorzata
Szmidt, Aleksander
Powiązania:
https://bibliotekanauki.pl/articles/2076079.pdf
Data publikacji:
2020
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
dolina subglacjalna
Zlodowacenie Wartanii/Saalii
osady wodnolodowcowe
deglacjacja powierzchniowa
diapir
subglacial valley
Wartanian/Saalian Glaciation
glaciofluvial sediments
areal deglaciation
Opis:
The subject of the analysis was a tunnel valley, weakly outlined in the landscape, located in central Poland, between Łódź and the Pilica valley to the west of Tomaszów Mazowiecki. The Miazga and lower Wolbórka flow along this valley. It is a 45-kilometre-long landform, mostly buried, partially covered with fluvial, slope and aeolian sediments, developed on a substratum characterised by varied palaeorelief and lithology. Sediments, which fill the valley, have variable thickness (10-100 m) and a non-flattened bottom gradient line, which indicates the possibility of water flow under hydrostatic pressure in a tunnel valley. Several segments of the channel cut into the Quaternary background. The filling consists mostly of glaciofluvial shallow braided rivers with average to low flow energy. In sedimentological terms, the deposits show significant similarity to the material of glaciofluvial kames found in the Łódź region. The authors believe there is a link between the accumulation in the tunnel valley and a particular variety of areal deglaciation, which was responsible for the formation of the fairly unvarying glacial relief. In outcrops in Łaznowska Wola, including the ones located in a hill that had been previously interpreted as an esker, some intrusive diapiric structures were documented, which reached the land surface. Thesefolded and locally disjunctive disturbances provide evidence for deformational origin of the hill.
Źródło:
Przegląd Geologiczny; 2020, 68, 7; 584--600
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł

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