The Response of the Rivers of NW Greece to Late Quaternary Neotectonics, as Interpreted from Detrita...
The Response of the Rivers of NW Greece to Late Quaternary Neotectonics, as Interpreted from Detrital Petrology
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Basel: MDPI AG
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English
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Basel: MDPI AG
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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 transverse grabens. This study assesses the impact...
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Full title
The Response of the Rivers of NW Greece to Late Quaternary Neotectonics, as Interpreted from Detrital Petrology
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TN_cdi_doaj_primary_oai_doaj_org_article_e54c5976dbb74b61a1aec39d120c7cc0
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https://devfeature-collection.sl.nsw.gov.au/record/TN_cdi_doaj_primary_oai_doaj_org_article_e54c5976dbb74b61a1aec39d120c7cc0
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ISSN
2076-3263
E-ISSN
2076-3263
DOI
10.3390/geosciences12110392
