The evaluation of geological structures by the vector analysis of valley axes
Identifikátory výsledku
Kód výsledku v IS VaVaI
<a href="https://www.isvavai.cz/riv?ss=detail&h=RIV%2F00088382%3A_____%2F14%3AN0000001" target="_blank" >RIV/00088382:_____/14:N0000001 - isvavai.cz</a>
Výsledek na webu
<a href="https://www.schweizerbart.de/papers/zfg/detail/58/82764/The_evaluation_of_geological_structures_by_the_vector_analysis_of_valley_axes" target="_blank" >https://www.schweizerbart.de/papers/zfg/detail/58/82764/The_evaluation_of_geological_structures_by_the_vector_analysis_of_valley_axes</a>
DOI - Digital Object Identifier
<a href="http://dx.doi.org/10.1127/0372-8854/2013/0113" target="_blank" >10.1127/0372-8854/2013/0113</a>
Alternativní jazyky
Jazyk výsledku
angličtina
Název v původním jazyce
The evaluation of geological structures by the vector analysis of valley axes
Popis výsledku v původním jazyce
The paper describes the methodology of evaluating geological structures by the vector analysis of valley axes. Both geological structures and valley axes were determined by the azimuth and the dip which corresponds with the angle of the slope in the selected catchment in the central Czech Republic. The determination of the dip of valley axes has formed a base for the quantitative classification of valley axes analogous to geological structures. The following five types of valley axes were distinguished: sub-horizontal, gently inclined, moderately inclined, steeply inclined and sub-vertical. The orientations of both the valley axes and the geological structures were evaluated by the construction of outline diagrams in the programme Spheristat. The directions of valley axes were compared with geological structures by the statistical relationship using the chi square test. The directions of sub-horizontal valley axes correspond with the dip azimuth of foliations in contrast to the dip azimuth of joints in the model area. The evaluation of geological structures by the vector analysis of valley axes is practicable in all kinds of landscape.
Název v anglickém jazyce
The evaluation of geological structures by the vector analysis of valley axes
Popis výsledku anglicky
The paper describes the methodology of evaluating geological structures by the vector analysis of valley axes. Both geological structures and valley axes were determined by the azimuth and the dip which corresponds with the angle of the slope in the selected catchment in the central Czech Republic. The determination of the dip of valley axes has formed a base for the quantitative classification of valley axes analogous to geological structures. The following five types of valley axes were distinguished: sub-horizontal, gently inclined, moderately inclined, steeply inclined and sub-vertical. The orientations of both the valley axes and the geological structures were evaluated by the construction of outline diagrams in the programme Spheristat. The directions of valley axes were compared with geological structures by the statistical relationship using the chi square test. The directions of sub-horizontal valley axes correspond with the dip azimuth of foliations in contrast to the dip azimuth of joints in the model area. The evaluation of geological structures by the vector analysis of valley axes is practicable in all kinds of landscape.
Klasifikace
Druh
J<sub>imp</sub> - Článek v periodiku v databázi Web of Science
CEP obor
—
OECD FORD obor
10505 - Geology
Návaznosti výsledku
Projekt
—
Návaznosti
V - Vyzkumna aktivita podporovana z jinych verejnych zdroju
Ostatní
Rok uplatnění
2014
Kód důvěrnosti údajů
S - Úplné a pravdivé údaje o projektu nepodléhají ochraně podle zvláštních právních předpisů
Údaje specifické pro druh výsledku
Název periodika
Zeitschrift für Geomorphologie
ISSN
0372-8854
e-ISSN
1864-1687
Svazek periodika
58
Číslo periodika v rámci svazku
2
Stát vydavatele periodika
DE - Spolková republika Německo
Počet stran výsledku
15
Strana od-do
201-215
Kód UT WoS článku
000337116900005
EID výsledku v databázi Scopus
2-s2.0-84973467738