Tectonically controlled drainage evolution in Lokris (Central Greece)


Η. ΜΑΡΙΟΛΑΚΟΣ
Χ. ΚΡΑΝΗΣ
Χ. ΜΑΡΟΥΚΙΑΝ
Ι. ΦΟΥΝΤΟΥΛΗΣ
Résumé

This paper presents the results of our research in the area of Lokris (Central Greece), regarding the relationship between the neotectonic structures and the response of the drainage network, which is found to be tectonically controlled to a great degree. Neotectonic mapping, geometrical and kinematic analysis, and morphotectonic investigation have shown that the local neotectonic grain is attributable to torsional deformation.

Article Details
  • Rubrique
  • Tectonics
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Biographie de l'auteur
Χ. ΜΑΡΟΥΚΙΑΝ, Τομέας Γεωγραφίας - Κλιματολογίας, Πανεπιστήμιο Αθηνών

University of Athens

Références
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MARIOLAKOS, I., FOUNTOULIS, I., LOGOS, Ε., LOZIOS, S., 1991. Methods to study torsional neotectonic deformation. The case of Kalamata area SW Peloponnessus, Greece. In Ch. Qingxuan (ed.) Proc. Regional Crustal Stability and Geological Hazards, IGCP project 250, 3, 15-21, Inst. Geomechanics, Chinese Academy of Geological Sciences CAGS, Beijing.
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