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Wyświetlanie 1-3 z 3
Tytuł:
Litologiczno-strukturalne uwarunkowania rzeźby Sudetów
Lithological and structural control on the relief of the Sudetes.
Autorzy:
Migoń, P.
Placek, A.
Powiązania:
https://bibliotekanauki.pl/articles/2075095.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
rock control
structural geomorphology
rock strength
Sudetes
geomorfologia strukturalna
skały
spękania
Sudety
Opis:
The geomorphological landscape of the Sudetes consists of elements of diverse origin. While the gross features of relief are best attributed to up- and downfaulting in the late Cenozoic, landform diversity at a smaller scale results mainly from selective long-term denudation controlled by rock properties. The occurrence of rock- and structure-controlled landforms has long been noted in the Sudetes, but their identification remained at a rather descriptive level. Recent work involving an analysis of digital elevation models, combined with field-based determination of rock strength using Schmidt hammer helped to refine some previous concepts and to identify further relationships between rocks and relief at a medium scale. Many residual convex landforms (hills, ridges) are associated with rocks of markedly higher strength than in the surroundings. Differences in elevations which may be attributed to rock factor, attain 400–500 m, which is a figure comparable with minor fault-bounded horsts. Extensive tracts of low relief are partly rock-controlled too, as they are best developed where adjacent rock complexes show similar strength, whether high or low. By contrast, the presence of escarpments cutting across rock masses of comparable strength on both sides appears to point to faulting as the topography-controlling factor.
Źródło:
Przegląd Geologiczny; 2014, 62, 1; 36--43
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Rola zróżnicowania wytrzymałości skał w genezie rzeźby Masywu Ślęży (Przedgórze Sudeckie)
The role of spatial variability in rock strength in the origin of relief of the Ślęża Massif (Sudetic Foreland)
Autorzy:
Placek, A.
Powiązania:
https://bibliotekanauki.pl/articles/2074511.pdf
Data publikacji:
2007
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
masyw Ślęży
skała wytrzymała
pochodzenie rzeźby terenu
wiertarka Schmidta
Ślęża Massif
rock strength
relief origin
Schmidt hammer
Opis:
This article presents the results of rock hardness tests conducted in the Ślęża Massif to decipher the relationships between the geological structure and relief. It has been shown that all rock types of the massif represent similar mechanical strength. The highest mean strength was found in granite of the western slopes and the foothills of Mt. Ślęża, whereas the lowest strength is typical of gabbro from the central part of the massif, its summit and the eastern and southern slopes. Thus, the traditional concept emphasizing gabbro as being the most resistant rock has not been confirmed. There is also no evidence of higher strength of rocks within the massif, as compared to those in most of its surroundings. Variable mechanical strength is probably responsible for slope mesorelief (mid-slope benches and ridge lines), yet the hypothesis that the resistance of gabbro changes perpendicularly to the contact with granitoid intrusion has not received support. Higher mean Schmidt hammer rebound values and lower standard deviation occurring below 450 m a.s.l. are interpreted as a result of interaction between the structural factor and glacial exaration during the Odra Glaciation.
Źródło:
Przegląd Geologiczny; 2007, 55, 10; 861-869
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
Tytuł:
Wpływ cech strukturalnych piaskowców fliszowych z Mucharza (Beskid Mały) na procesy pękania w warunkach jednoosiowego ściskania
The influence of the structural features in the Krosno Sandstones of Mucharz (Little Beskids) on fracture processes under uniaxial compression conditions
Autorzy:
Pieczara, Ł.
Powiązania:
https://bibliotekanauki.pl/articles/2074265.pdf
Data publikacji:
2014
Wydawca:
Państwowy Instytut Geologiczny – Państwowy Instytut Badawczy
Tematy:
anizotropia
flisz
pękanie
piaskowce krośnieńskie
fala podłużna
obciążenie punktowe
wytrzymałość skał
anisotropy
flysch
fracture
Krosno Sandstones
longitudinal wave
point load test
rock mechanics
strength
thin-section
Opis:
The fracture processes of the Krosno Sandstones of Mucharz, southern Poland, were analysed to determine its relation to orientation of the structural features of the rock. The research putted focused estimating influence of characteristic structural features of the rock (arrangement of laminations plane and direction of arrangement of grains). In the initial stage of research, ultrasonic longitudinal wave propagation speed (Vp) tests were carried out on samples flysch sandstones. The results of the tests were analysed to determine effects of characteristic structural features of the rock on obtained values of longitudinal wave propagation speed (Vp), using on variability of obtained results depending on orientation of mineral elements. In the second part of the study, the point load test was used to determine rock strength under uniaxial compression conditions. In order to estimate uniaxial compressive strength, index-to-strength conversion factors were used. The point load test apparatus and procedure enables economical testing of rock samples in either a field or laboratory setting. Last part of the research was application of computer methods enabled to show technique of analysis microscopic images of the thin – section flysch sandstones samples, tested on point load tests and filled with a staining substance. The study elucidated the structural controls of the fracture processes of the flysch sandstones from Gorka – Mucharz quarry.
Źródło:
Przegląd Geologiczny; 2014, 62, 10/2; 680--686
0033-2151
Pojawia się w:
Przegląd Geologiczny
Dostawca treści:
Biblioteka Nauki
Artykuł
    Wyświetlanie 1-3 z 3

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