The Response of the Rivers of NW Greece to Late Quaternary Neotectonics, as Interpreted from Detrital Petrology

The modern drainage systems of the fold and thrust belt of the external Hellenide orogen of NW Greece are principally orogen-parallel. Late Quaternary changes in river courses have resulted from neotectonic deformation associated with the Katouna–Stamna fault and with footwall uplift in developing t...

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Bibliographic Details
Main Authors: David J. W. Piper, Georgia Pe-Piper
Format: Article
Language:English
Published: MDPI AG 2022-10-01
Series:Geosciences
Subjects:
Online Access:https://www.mdpi.com/2076-3263/12/11/392