Quaternary geology, geomorphology and tectonics in the Ogosta river valley system, the Danubian plain (Bulgaria)

 
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Journal part (EN)
Scientific article (EN)
2001 (EN)
Quaternary geology, geomorphology and tectonics in the Ogosta river valley system, the Danubian plain (Bulgaria) (EN)
ANGELOVA, D.
The Quaternary in the Ogosta River valley system (the Danubian plain) is represented by various genetic types of continental Quaternary sediments (eolian, alluvial, deluvial, proluvial). They lie on a diverse pre-Quaternary base. It is uneven and with various denudation. The accepted correlation schemes are based on local data in which the tectonic factor and duration of deformation have not been accounted for. The present work considers the complex results obtained during the investigation of the Quaternary sediments and formations. The filling consists of clayey-sandy or calcareous-sandy materials, coloured in rusty nuances by iron hydroxides. Their age has been determined on the basis of the found fauna: Elephas meridionalis Nesti,Anancus arvernensis Cr. et Gob (Bakalov, Nikolov, 1962). (EN)
info:eu-repo/semantics/article
info:eu-repo/semantics/publishedVersion
geomorphology (EN)
lithology (EN)
Quaternary geology (EN)
tectonics (EN)
Geological Society of Greece
Bulletin of the Geological Society of Greece
General and Structural Geology
Δελτίο της Ελληνικής Γεωλογικής Εταιρίας
English
2001-01-01
https://ejournals.epublishing.ekt.gr/index.php/geosociety/article/view/16943
Geological Society of Greece (EN)
0438-9557
2529-1718
Δελτίο της Ελληνικής Γεωλογικής Εταιρείας; Τόμ. 34 Αρ. 1 (2001): 9o διεθνές Συνέδριο της ΕΓΕ; 55-60 (EL)
Bulletin of the Geological Society of Greece; Vol. 34 No. 1 (2001): 9th International Conference of the Geological Society of Greece; 55-60 (EN)
https://creativecommons.org/licenses/by-nc/4.0 (EN)
Copyright (c) 2018 D. ANGELOVA (EN)



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