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Rola brył martwego lodu w morfogenezie Kotliny Grudziądzkiej i Basenu Świeckiego : formy rzeźby i osady 死冰固体在Grudzińdzka盆地和西威基盆地形态发生中的作用：雕塑和沉积物的形式
Landform Analysis Pub Date : 2014-09-12 DOI: 10.12657/LANDFANA.025.005
J. Kordowski
{"title":"Rola brył martwego lodu w morfogenezie Kotliny Grudziądzkiej i Basenu Świeckiego : formy rzeźby i osady","authors":"J. Kordowski","doi":"10.12657/LANDFANA.025.005","DOIUrl":"https://doi.org/10.12657/LANDFANA.025.005","url":null,"abstract":"","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"25 1","pages":"43-54"},"PeriodicalIF":0.0,"publicationDate":"2014-09-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210438","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
Geneza rzeźby glacjalnej i dynamika ostatniego lądolodu w rejonie Górzna i Lidzbarka (północno-środkowa Polska) na podstawie analiz geoprzestrzennych 基于地理空间分析的Górzno和Lidzbarko地区（波兰中北部）冰川雕塑的起源和最后一座冰川的动力学
Landform Analysis Pub Date : 2014-09-12 DOI: 10.12657/LANDFANA.025.012
M. Sobiech, W. Wysota
{"title":"Geneza rzeźby glacjalnej i dynamika ostatniego lądolodu w rejonie Górzna i Lidzbarka (północno-środkowa Polska) na podstawie analiz geoprzestrzennych","authors":"M. Sobiech, W. Wysota","doi":"10.12657/LANDFANA.025.012","DOIUrl":"https://doi.org/10.12657/LANDFANA.025.012","url":null,"abstract":"","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"25 1","pages":"135-142"},"PeriodicalIF":0.0,"publicationDate":"2014-09-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210635","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
Próba rekonstrukcji pierwotnej rzeźby obszaru Zespołu Staromiejskiego w Toruniu i jego bliskich przedmieść na podstawie geoinformacji geologicznej i historycznej 根据地质和历史信息，试图重建托伦老城建筑群及其近郊的原始雕塑
Landform Analysis Pub Date : 2014-09-12 DOI: 10.12657/LANDFANA.025.010
Pawe ³ Molewski, Włodzimierz Juśkiewicz
{"title":"Próba rekonstrukcji pierwotnej rzeźby obszaru Zespołu Staromiejskiego w Toruniu i jego bliskich przedmieść na podstawie geoinformacji geologicznej i historycznej","authors":"Pawe ³ Molewski, Włodzimierz Juśkiewicz","doi":"10.12657/LANDFANA.025.010","DOIUrl":"https://doi.org/10.12657/LANDFANA.025.010","url":null,"abstract":"","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"25 1","pages":"115-124"},"PeriodicalIF":0.0,"publicationDate":"2014-09-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210575","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 8
Transformacja form korytowych na przykładzie aluwiów piaskodennych rzek roztokowych środkowego vistulianu w Kotlinie Toruńskiej 河床形态的转变——以托伦盆地维斯图连中部的沙冲积层河流为例
Landform Analysis Pub Date : 2014-09-12 DOI: 10.12657/LANDFANA.025.015
P. Weckwerth
{"title":"Transformacja form korytowych na przykładzie aluwiów piaskodennych rzek roztokowych środkowego vistulianu w Kotlinie Toruńskiej","authors":"P. Weckwerth","doi":"10.12657/LANDFANA.025.015","DOIUrl":"https://doi.org/10.12657/LANDFANA.025.015","url":null,"abstract":"","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"25 1","pages":"169-177"},"PeriodicalIF":0.0,"publicationDate":"2014-09-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210668","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Postglacjalne zmiany środowiska przyrodniczego na Wysoczyźnie Dobrzyńskiej zapisane w profilu osadów biogenicznych w Piotrkowie Piotrków生物成因沉积物剖面中记录的多布日恩斯卡高地自然环境的冰川后变化
Landform Analysis Pub Date : 2014-09-12 DOI: 10.12657/LANDFANA.025.001
Wojciech Gamrat, L. Andrzejewski, Iwona Krześlak
{"title":"Postglacjalne zmiany środowiska przyrodniczego na Wysoczyźnie Dobrzyńskiej zapisane w profilu osadów biogenicznych w Piotrkowie","authors":"Wojciech Gamrat, L. Andrzejewski, Iwona Krześlak","doi":"10.12657/LANDFANA.025.001","DOIUrl":"https://doi.org/10.12657/LANDFANA.025.001","url":null,"abstract":"Piotrkowo site is located in the western part of the Dobrzyn Plateau. Detailed pollen analysis of the Piotrkowo I core enabled a reconstruction of environmental conditions change over last several thousand years. The results indicated three different stages of the organic sedimentation, two limnic and one terrestrial. The first stage of Plenivistulian age lake is recorded in organic silt sediment, partly laminated. The second stage contains traces of Holocene age lake preserved in carbonate gyttja sediment. The last phase includes a record of dynamic changes in the groundwater level recorded in terrestrial sediments - highly decomposed peat and organic loam.","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"25 1","pages":"3-11"},"PeriodicalIF":0.0,"publicationDate":"2014-09-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210365","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 3
Morfologia i etapy rozwoju parowu w Uściu koło Chełmna Chełmno附近Uscie蒸汽发育的形态和阶段
Landform Analysis Pub Date : 2014-09-12 DOI: 10.12657/LANDFANA.025.002
T. Jaworski, Włodzimierz Juśkiewicz
{"title":"Morfologia i etapy rozwoju parowu w Uściu koło Chełmna","authors":"T. Jaworski, Włodzimierz Juśkiewicz","doi":"10.12657/LANDFANA.025.002","DOIUrl":"https://doi.org/10.12657/LANDFANA.025.002","url":null,"abstract":"","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"25 1","pages":"13-20"},"PeriodicalIF":0.0,"publicationDate":"2014-09-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210373","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 1
Charakterystyka środowisk depozycyjnych Jeziora Czechowskiego i jego otoczenia 切丘斯基湖及其周边沉积环境特征
Landform Analysis Pub Date : 2014-09-12 DOI: 10.12657/LANDFANA.025.006
J. Kordowski, M. Błaszkiewicz, Mateusz Kramkowski, Michał Słowiński, Sebastian Tyszkowski, Achim Brauer, D. Brykała, P. Gierszewski, P. Lamparski, Monika Lutyńska, J. Mirosław-Grabowska, A. Noryskiewicz, Milena Obremska, Florian Ott, S. Wulff, Izabela Zawiska
{"title":"Charakterystyka środowisk depozycyjnych Jeziora Czechowskiego i jego otoczenia","authors":"J. Kordowski, M. Błaszkiewicz, Mateusz Kramkowski, Michał Słowiński, Sebastian Tyszkowski, Achim Brauer, D. Brykała, P. Gierszewski, P. Lamparski, Monika Lutyńska, J. Mirosław-Grabowska, A. Noryskiewicz, Milena Obremska, Florian Ott, S. Wulff, Izabela Zawiska","doi":"10.12657/LANDFANA.025.006","DOIUrl":"https://doi.org/10.12657/LANDFANA.025.006","url":null,"abstract":"","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"25 1","pages":"55-75"},"PeriodicalIF":0.0,"publicationDate":"2014-09-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210446","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
Zróżnicowanie facjalne glin jako wskaźnik fluktuacji ciśnienia wód subglacjalnych na kontakcie lodu i podłoża podczas zlodowacenia wisły w północnej części Pojezierza Dobrzyńskiego 多布日恩斯基湖区北部的粘土表面变化是冰川作用期间冰和地面上冰下水压波动的指标
Landform Analysis Pub Date : 2014-09-12 DOI: 10.12657/LANDFANA.025.011
Włodzimierz Narloch, J. Wojciechowska, Alicja Osowicka, W. Wysota, J. Piotrowski, M. Sobiech
{"title":"Zróżnicowanie facjalne glin jako wskaźnik fluktuacji ciśnienia wód subglacjalnych na kontakcie lodu i podłoża podczas zlodowacenia wisły w północnej części Pojezierza Dobrzyńskiego","authors":"Włodzimierz Narloch, J. Wojciechowska, Alicja Osowicka, W. Wysota, J. Piotrowski, M. Sobiech","doi":"10.12657/LANDFANA.025.011","DOIUrl":"https://doi.org/10.12657/LANDFANA.025.011","url":null,"abstract":"Sedimentological analyses were performed on glacial till of the Weichselian glaciation in two field sites (Przeszkoda and Oborki) which are located in northern part of the Dobrzyn Lakeland. During the last glaciation this area was covered by the Vistula ice lobe which development has been determined by the Vistula Ice Stream. A multi-proxy approach including a study of sedimentary features, grain size, petrographic composition, till fabric and till micromorphology was used in reconstruction of till formation and ice movement mechanisms. Analysed tills are massive and stratified. We suggest existing of complex and temporally variable conditions under the Vistula ice lobe, probably caused by subglacial water fluctuations. Ice movement was caused by a combination of bed deformation and basal sliding.","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"25 1","pages":"125-133"},"PeriodicalIF":0.0,"publicationDate":"2014-09-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210622","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 2
Próba modelowania prędkości przepływu wody oraz rozprzestrzeniania się zanieczyszczeń w jeziorze Gopło 试图模拟Gopło湖的水流速度和污染物扩散
Landform Analysis Pub Date : 2014-09-12 DOI: 10.12657/LANDFANA.025.003
Włodzimierz Juśkiewicz
{"title":"Próba modelowania prędkości przepływu wody oraz rozprzestrzeniania się zanieczyszczeń w jeziorze Gopło","authors":"Włodzimierz Juśkiewicz","doi":"10.12657/LANDFANA.025.003","DOIUrl":"https://doi.org/10.12657/LANDFANA.025.003","url":null,"abstract":"","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"25 1","pages":"21-27"},"PeriodicalIF":0.0,"publicationDate":"2014-09-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210383","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 3
Wpływ procesów denudacji na właściwości osadów wypełniających zagłębienia między krętymi wałami z erozji wód subglacjalnych w okolicy Zbójna (Pojezierze Dobrzyńskie) 剥蚀过程对Zbójn地区（Dobrzyńskie湖区）冰下水域侵蚀形成的填充竖井之间凹坑的沉积物特性的影响
Landform Analysis Pub Date : 2014-09-12 DOI: 10.12657/LANDFANA.025.004
M. Karasiewicz, P. Hulisz, M. Świtoniak
{"title":"Wpływ procesów denudacji na właściwości osadów wypełniających zagłębienia między krętymi wałami z erozji wód subglacjalnych w okolicy Zbójna (Pojezierze Dobrzyńskie)","authors":"M. Karasiewicz, P. Hulisz, M. Świtoniak","doi":"10.12657/LANDFANA.025.004","DOIUrl":"https://doi.org/10.12657/LANDFANA.025.004","url":null,"abstract":"The research was conducted within a test field of 1 km2 located near Zbójno, that lies in the south-eastern part of the Dobrzyń Lakeland. The objective of the research was to analyze the effect of natural and anthropogenic denudation on the properties of sediments in depressions between glacial curvilineations. Five types of deposits were identified in the studied depressions. These depressions are filled with sediments sequences which are closely associated with natural processes and long-term extensive farming. The degree and the range of transformations of deposits and depressions depend largely on their morphometric characteristics of these depressions. Compared with sediments building the ridge of a glacial curvilineation, the deposits of the analysed depressions were characterised by significantly different chemical composition, which clearly indicates their function as sediment traps.","PeriodicalId":30719,"journal":{"name":"Landform Analysis","volume":"25 1","pages":"29-42"},"PeriodicalIF":0.0,"publicationDate":"2014-09-12","publicationTypes":"Journal Article","fieldsOfStudy":null,"isOpenAccess":false,"openAccessPdf":"","citationCount":null,"resultStr":null,"platform":"Semanticscholar","paperid":"66210425","PeriodicalName":null,"FirstCategoryId":null,"ListUrlMain":null,"RegionNum":0,"RegionCategory":"","ArticlePicture":[],"TitleCN":null,"AbstractTextCN":null,"PMCID":"","EPubDate":null,"PubModel":null,"JCR":null,"JCRName":null,"Score":null,"Total":0}
引用次数: 7
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