Results 11 to 20 of about 6,721 (174)
Geological parameters for diluvium and flysch.
This work is mainly intended to investigate the flysch landslide reinforcement measures used in the Smokovac-Mateševo section of the North-South Expressway project in Montenegro.
Weidong Wang (321040) +3 more
core +1 more source
Role of Saravan Thrust Fault on Formation and Development of Saravan Catchment Basin [PDF]
Development of drainage basins has close relation with geomorphologic and geologic parameters. Therefore, study the relation between structural parameters like faults and development of drainage basins has greatly considered in hydrology and hydrogeology
Ali Asqar Moridi Farimani +1 more
doaj +1 more source
Caracterização geoquímica do Grupo do Flysch do Baixo Alentejo (Zona Sul Portuguesa): resultados preliminares [PDF]
O Grupo do Flysch do Baixo Alentejo (GFBA) é um dos domínios da Zona Sul Portuguesa (ZSP), sendo constituído por sedimentos turbidíticos profundos, com uma espessura superior a 5 km (Oliveira, 1990)
Oliveira, José Tomás +3 more
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Biostratigraphical study of Lower Cretaceous Kašajina river beds and its importance for geology of NE Serbia [PDF]
This article presents results of detailed palynological study in the Lower Cretaceous Kašajina River Beds (Klokočevac, NE Serbia) and its importance for the geology of NE Serbia.
Ercegovac Marko +2 more
doaj +1 more source
Relation between relief and Badland spatial distribution in the Paleogene Pazin Basin, Croatia
Badlands are specific landforms characterized by intense denudation processes. Their occurrence is mainly associated with clay-like materials and semi-arid and Mediterranean climates.
Iris Bostjančić +3 more
doaj +1 more source
This research focuses on the analysis of soil-water interaction at the carbonate-flysch contact on the Istrian peninsula in Croatia. As a result of the interaction of surface and groundwater and the position of flysch and carbonate rocks in the ...
Sanja Dugonjić Jovančević +3 more
doaj +1 more source
Baseflow separation was performed for 42 small catchments completely built up of either crystalline rocks or folded/unfolded Paleogene flysch rocks. Three different methods were applied—Local minimum (BFI), Kille’s and Rambert’s. Mean total annual runoff
Rudolf Dugovič +3 more
doaj +1 more source
Caracterização geoquímica da formação brejeira (grupo do Flysch do Baixo Alentejo): resultados preliminares [PDF]
A Formação Brejeira é a unidade litoestratigráfica mais recente do Grupo do Flysch do Baixo Alentejo consistindo, essencialmente, de grauvaques e quartzovaques de natureza turbidítica intercalados com xistos argilosos. A idade da Fm.
Oliveira, José Tomás +4 more
core +1 more source
he aim of this work is the stratigraphic revision of the sequences outcropping on the southwestern side of the M. Mia — M. Matajur anticline. This area, until now, was poorly studied from a geological point of view.
CAMILLA PIRINI RADRIZZANI +2 more
doaj
Bankfull widths in steep headwaters of the flysch Carpathians [PDF]
Bankfull widths of steep headwater channels were examined in the Western Carpathian flysch midmountains. The criteria of the top of banks, scoured lines and presence of bank vegetation were helpful in the bankfull width determination.
Tomáš Galia, Václav Škarpich
doaj +1 more source

