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Wiley, Earth Surface Processes and Landforms, 4(45), p. 1013-1027, 2020

DOI: 10.1002/esp.4795

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A GIS method to identify flat surfaces and restore relict fluvial long‐profiles from terrace remnants gives new clues on how large basins respond to endorheic–exorheic transitions (Duero basin, Iberian Peninsula)

This paper was not found in any repository, but could be made available legally by the author.
This paper was not found in any repository, but could be made available legally by the author.

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