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...
Main Authors: | , , |
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Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Alexandria, Va. : GeoScienceWorld
2021
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Subjects: | |
Online Access: | https://www.repo.uni-hannover.de/handle/123456789/11277 https://doi.org/10.15488/11191 |