The occurrence of several orders of morphologically linked fluvial and marine terraces clearly documents that the regional geodynamic process was mainly governed by eustasy, though Late Quaternary tectonics certainlyplayed an important role in the evolution of the area. The present research is devoted to recognise, separate and possibly quantify the tectonic effects within the area.

Morphological evidence of Late Quaternary thrusting in the Bradanic Foredeep

Caputo R.
Primo
Membro del Collaboration Group
;
BIANCA, Marcello
Secondo
Membro del Collaboration Group
2005

Abstract

The occurrence of several orders of morphologically linked fluvial and marine terraces clearly documents that the regional geodynamic process was mainly governed by eustasy, though Late Quaternary tectonics certainlyplayed an important role in the evolution of the area. The present research is devoted to recognise, separate and possibly quantify the tectonic effects within the area.
2005
Caputo, R.; Bianca, Marcello
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Utilizza questo identificativo per citare o creare un link a questo documento: https://hdl.handle.net/11392/2391981
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