Fluvial system response to tectonically induced base-level change during the late-Quaternary: The Rio Alias southeast Spain

The Rio Alias of southeast Spain crosses a major tectonically active structure, the Carboneras Fault Zone, within the central portion of the drainage basin. The fault originated in the mid-Miocene and has c.40 km of strike-slip offset. The impact of late Quaternary movement along the fault zone on t...

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Veröffentlicht in:	Geomorphology (Amsterdam, Netherlands) Netherlands), 2008-08, Vol.100 (1), p.180-192
Hauptverfasser:	Maher, Elizabeth, Harvey, Adrian M.
Format:	Artikel
Sprache:	eng
Schlagworte:	Fluvial geomorphology/sedimentology Quaternary Southeast Spain Tectonics
Online-Zugang:	Volltext
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