Article ID Journal Published Year Pages File Type
9526991 Tectonophysics 2005 26 Pages PDF
Abstract
The older river drainage system has also been modified by Late Pliocene-Quaternary folding, thrusting and monoclinal tilting along the Pericarpathian orogenic front and by reactivated transverse high angle basement faults, which cross the Eastern Carpathian foreland.
Keywords
Related Topics
Physical Sciences and Engineering Earth and Planetary Sciences Earth-Surface Processes
Preview
Late Miocene-Quaternary volcanism, tectonics and drainage system evolution in the East Carpathians, Romania
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