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Wyszukujesz frazę "glaciotectonic" wg kryterium: Temat


Wyświetlanie 1-2 z 2
Tytuł:
Reconstruction of ice sheet movement from the orientation of linearglacial landforms and glaciotectonic deformations near Kronowo (western Mazury, Poland)
Autorzy:
Morawski, W.
Powiązania:
https://bibliotekanauki.pl/articles/2058830.pdf
Data publikacji:
2003
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
Mazury
Vistulian Glaciation
ice sheet movement direction
morpholineaments
glaciotectonic
Opis:
Ice sheet movement in northeastern Poland is reconstructed from analysis of the spatial orientation of glacial landforms and glaciotectonic deformations. The orientations of both positive and negative glacial landforms (morpholineaments) of the Vistulian Glaciation were analysed. These landforms form 4 sets and follow an original crevasse system (joint net) within the ice sheet, probably resulting from horizontal stress exerted as the ice advanced from the north. Esker deposits have been glaciotectonically deformed to form a compressional fan fold, due to limited movement of the ice sheet prior to deglaciation. This movement caused the ice crevasses to be tightened and cut by strike-slip faults. Movement here was from the NNW, as determined from the orientation of deformations. Thus, the ice-flow direction changed at least by 10° during the last phase of the Vistulian Glaciation. If the ice rotated the northeastern portion of the esker, this change may have amounted to 30°.
Źródło:
Geological Quarterly; 2003, 47, 4; 339--356
1641-7291
Pojawia się w:
Geological Quarterly
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Warmińska prowincja paleogeograficzna plejstocenu (północno-wschodnia Polska)
The Warmia Palaeogeographic Province of the Pleistocene (north–eastern Poland)
Autorzy:
Morawski, W.
Powiązania:
https://bibliotekanauki.pl/articles/2074336.pdf
Data publikacji:
2005
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
plejstocen
palaeografia
stratygrafia
glacitektonika
morfolineament polodowcowy
prowincja paleogeograficzna
geofizyka
Warmia
Pleistocene
palaeogeography
stratigraphy
glaciotectonic structures
glacial morpholineaments
ice-sheet movement
geophysical methods
NE Poland
Opis:
The historic area of Warmia (western part of NE Poland) can be considered as a separate geological unit. In particular it applies to its Pleistocene sedimentary complex with a very limited occurrence of morainic deposits, commonly forming discontinuous horizons. Intermorainic deposits predominate, including mainly ice-dam lake deposits which occur at different levels. The sub-Pleistocene relief variations reach up to 400 m, with glaciotectonic upthrustings of Neogene deposits extending to the topographic surface. The province area coincides with the Warmia ice-sheet lobe of the last glaciation (Main Stadial of the Vistulian Glaciation). The eastern boundary of the area is represented by an interlobe zone coincident with the western slope of the Mazury–Suwałki Anteclise. The boundary is a tectonic discontinuity zone extending down to the crystalline basement. The eastern, anteclise area was stable during the Pleistocene, while the area of Warmia (Peri-Baltic Syneclise) was unstable mainly due to cyclic ice-sheet loads which resulted in subsidence in the Warmia region. It, in turn, caused a bending of the ice sheet body, movement acceleration and a change in ice flow direction in Warmia. During interglacials, relaxation uplifting movements triggered stronger erosional processes. These movements were dependent on surface relief, stimulating the formation of deeply rooted glaciotectonic structures.
Źródło:
Przegląd Geologiczny; 2005, 53, 6; 477--488
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-2 z 2

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