Content uploaded by Kord Ernstson
Author content
All content in this area was uploaded by Kord Ernstson on Mar 20, 2022
Content may be subject to copyright.
Transpression and Transtension Impact Cratering Features: the Steinheim, Saarlouis (both Germany) and Singra-Jiloca (Spain) Cases.
... After the impact, proposed to have occurred in the Pleistocene epoch [2], this plate movement caused the original, presumably round crater, to be disrupted and deformed, even possibly made smaller. Consequently, transpressional ridges and transtensional troughs [3] from the modification stage of the cratering process, can still be observed on land in the Digital Terrain Model (Figure 4), and on the adjacent sea floor of the receding Aegean plate ( Figure 3). ...
ResearchGate has not been able to resolve any references for this publication.