Spatiotemporal history of fault–fluid interaction in the Hurricane fault, western USA
<p>The Hurricane fault is a <span class="inline-formula">∼250</span> km long, west-dipping, segmented normal fault zone located along the transition between the Colorado Plateau and the Basin and Range tectonic provinces in the western USA. Extensive evidence o...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2020-11-01
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| Series: | Solid Earth |
| Online Access: | https://se.copernicus.org/articles/11/1969/2020/se-11-1969-2020.pdf |