Wyniki wyszukiwania - BazTech

1

Stratighaphic position of tills in the Orłowo Cliff section (northern Poland): a new approach

Woźniak P. P., Sokołowski R. J., Czubla P., Fedorowicz S.

Studia Quaternaria

|

2018

|

Vol. 35, Nr 1

25--40

EN

The site at Orłowo Cliff was used to analyse the stratigraphic position and palaeogeographic interpretations of the properties and depositional conditions of two basal tills from the Late Pleistocene. A multi-proxy approach involved lithofacies, petrographic analysis of the fine gravel fraction, analyses of indicator erratics and till fabric. TL dating of intra-moraine deposits was used to determine depositional time frames of tills. The sediment profile at Orłowo Cliff shows a distinct reduction in number of Pleistocene units. Obtained dating results suggest the presence of Middle and Late Pleistocene fluvial units. The main issue discussed is the stratigraphic position of the older till (Unit O-4). It can be assumed that this till was deposited probably during the Middle Weichselian (MIS4). At Orłowo Horn the till of Unit O-4 reveals incorporation of the erratic material derived from an older till in the surrounded area (according to petrographic composition – probably from MIS 8). The younger till (Unit O-6) was deposited in the Late Weichselian (MIS 2). Moreover, the till of Unit O-6 is characterised by a significant shift towards the south-west in terms of the erratic origin in Unit O-4.

2

River response to climate and sea level changes during the Late Saalian/Early Eemian in northern Poland – a case study of meandering river deposits in the Chłapowo cliff section

Moskalewicz D., Sokołowski R. J., Fedorowicz S.

Geologos

|

2016

|

Vol. 22, No. 1

1--14

EN

Fluvial sediments in the Chłapowo cliff section were studied in order to reconstruct their palaeoflow conditions and stratigraphical position. Lithofacies, textural and palaeohydraulic analyses as well as luminescence dating were performed so as to achieve the aim of study. Sedimentary successions were identified as a record of point bar cycles. The fluvial environment probably functioned during the latest Saalian, shortly after the retreat of the Scandinavian Ice Sheet. Discharge outflow was directed to the northwest. The river used the older fluvioglacial valley and probably was directly connected to the Eem Sea. Good preservation and strong aggradation of point-bar cycles were related to a rapid relative base level rise. The meandering river sediments recognised showed responses to climate and sea level changes as illustrated by stratigraphical, morphological and sedimentological features of the strata described. The present study also revealed several insights into proper interpretation of meandering fluvial successions, in which the most important were: specific lithofacies assemblage of GSt (St, Sp) → Sl → SFrc → Fm (SFr) and related architectural elements: channel/sandy bedforms CH/SB → lateral accretion deposits LA → floodplain fines with crevasse splays FF (CS); upward-fining grain size and decreasing content of denser heavy minerals; estimated low-energy flow regime with a mean depth of 1.6–3.3 m, a Froude number of 0.2–0.4 and a sinuosity of 1.5.

3

Depositional conditions on an alluvial fan at the turn of the Weichselian to the Holocene – a case study in the Żmigród Basin, southwest Poland

Zieliński P., Sokołowski R. J., Fedorowicz S., Woronko B., Hołub B., Jankowski M., Kuc M., Tracz M.

Geologos

|

2016

|

Vol. 22, No. 2

105--120

EN

Presented are the results of research into the fluvio-aeolian sedimentary succession at the site of Postolin in the Żmigród Basin, southwest Poland. Based on lithofacies analysis, textural analysis, Thermoluminescence and Infrared-Optical Stimulated Luminescence dating and GIS analysis, three lithofacies units were recognised and their stratigraphic succession identified: 1) the lower unit was deposited during the Pleni-Weichselian within a sand-bed braided river functioning under permafrost conditions within the central part of the alluvial fan; 2) the middle unit is the result of aeolian deposition and fluvial redeposition on the surface of the fan during long-term permafrost and progressive decrease of humidity of the climate at the turn of the Pleni to the Late Weichselian; 3) the upper unit accumulated following the development of longitudinal dunes at the turn of the Late Weichselian to the Holocene; the development of dunes was interrupted twice by the form being stabilised by vegetation and soil development.

4

Climate evolution during the Pleniglacial and Late Glacial as recorded in quartz grain morphoscopy of fluvial to aeolian successions of the European Sand Belt

Woronko B., Zieliński P., Sokołowski R. J.

Geologos

|

2015

|

Vol. 21, No. 2

89--103

EN

We present results of research into fluvial to aeolian successions at four sites in the foreland of the Last Glacial Maximum, i.e., the central part of the “European Sand Belt”. These sites include dune fields on higher-lying river terraces and alluvial fans. Sediments were subjected to detailed lithofacies analyses and sampling for morphoscopic assessment of quartz grains. Based on these results, three units were identified in the sedimentary succession: fluvial, fluvio-aeolian and aeolian. Material with traces of aeolian origin predominate in these sediments and this enabled conclusions on the activity of aeolian processes during the Pleniglacial and Late Glacial, and the source of sediment supply to be drawn. Aeolian processes played a major role in the deposition of the lower portions of the fluvial and fluvio-aeolian units. Aeolian material in the fluvial unit stems from aeolian accumulation of fluvial sediments within the valley as well as particles transported by wind from beyond the valley. The fluvio-aeolian unit is composed mainly of fluvial sediments that were subject to multiple redeposition, and long-term, intensive processing in an aeolian environment. In spite of the asynchronous onset of deposition of the fluvio-aeolian unit, it is characterised by the greatest homogeneity of structural and textural characteristics. Although the aeolian unit was laid down simultaneously, it is typified by the widest range of variation in quartz morphoscopic traits. It reflects local factors, mainly the origin of the source material, rather than climate. The duration of dune-formation processes was too short to be reflected in the morphoscopy of quartz grains.

5

Stratigraphic position of fluvial and aeolian deposits in the Żabinko site (w Poland) based on TL dating

Zieliński P. P., Sokołowski R. J., Fedorowicz S., Jankowski M.

Geochronometria

|

2011

|

Vol. 38, no. 1

64-71

EN

The known from literature Żabinko site is situated in the Warta Pradolina, within the dune field occurring on the bifurcation terrace. In the site we found fluvial, fluvio-aeolian and aeolian deposits, paleosols, and organic infillings of the inactive river channels. The purpose of the study was to determine stratigraphic position of the deposit units distinguished on the basis of lithofacial analysis, pedological description and thermoluminescence dating. The obtained results well correspond to the previously published ones, and new units were also found.

6

Dynamika lobu Wisły podczas ostatniego zlodowacenia w świetle nowych badań

Wysota W., Molewski P., Sokołowski R. J.

Landform Analysis

|

2008

|

Vol. 9

264--266

7

Rola zlodowacenia warty w morfogenezie i wykształceniu osadów czwartorzędowych w NE części Wyżyny Wieluńskiej

Sokołowski R. J.

Przegląd Geologiczny

|

2002

|

Vol. 50, nr 5

431-436

PL

Osady czwartorzędowe na Wyżynie Wieluńskiej mają małą miąższość i nie tworzą ciągłej pokrywy. Jest to efekt wyżynnego charakteru badanego obszaru, przeważających ruchów wznoszących i spowodowanej nimi denudacji. Na badanym terenie dominują osady zlodowacenia warty podścielone miejscami osadami zlodowacenia odry i zlodowaceń sanu. Brak jednak organicznych osadów interglacjalnych, na podstawie których można by jednoznacznie określić ich wiek. Osady są genezy fluwioglacjalnej i glacjalnej, z późniejszymi przekształceniami w warunkach peryglacjalnych.