Postglacial slip distribution along the Teton normal fault (Wyoming, USA), derived from tectonically offset geomorphological features

Along the eastern front of the Teton Range, northeastern Basin and Range province (Wyoming, USA), well-preserved fault scarps that formed across moraines, river terraces, and other geomorphological features indicate that multiple earthquakes ruptured the range-bounding Teton normal fault after the L...

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Bibliographic Details
Main Authors: Hampel, Andrea, Hetzel, Ralf, Erdmann, Maria-Sophie
Format: Article in Journal/Newspaper
Language:English
Published: Alexandria, Va. : GeoScienceWorld 2021
Subjects:
USA
Online Access:https://www.repo.uni-hannover.de/handle/123456789/11277
https://doi.org/10.15488/11191