Sedimentation in the mid- Netherlands river area during the Late Weichselian.
article
Focusses on the distribution of river-dune deposits and overbank deposits (Hochfluthlehm), in the central Netherlands River Rhine area. They are assigned to the Lateglacial member of the Kreftenheye Formation. As a consequence of this lithological study a more precise picture can be presented of the changes from a Pleniglacial braided river system into a more channel-bound river system.-from Author
Topics
TNO Identifier
229496
Source
Geologie en Mijnbouw, 62(3), pp. 487-491.
Pages
487-491