Published November 2012
| public
Journal Article
The Plio-Quaternary uplift of the Sierra Nevada, mechanical causes and consequences
- Creators
- Le Pourhiet, Laetitia
- Saleeby, Jason B.
Abstract
The southern Sierra Nevada Mountains range rapidly uplifted at ≈ 3.5 Ma simultaneously with a pulse of basaltic volcanism. Xenoliths recovered from volcanics indicate that the range lost a dense crustal root after the Miocene. The vertical motions and removal of the root have been linked to a fast seismic velocity anomaly that extends ≈ 200 km into the mantle but is offset to the west of the range. With visco-elasto-plastic thermo-mechanical numerical models, we have tested the influence of crustal strength on the kinematics of removal and on the amount of associated uplift. We find that delamination of the dense root is the most likely mechanism for gravitational instability to occur.
Additional Information
© 2012 Geological Society of America.Additional details
- Eprint ID
- 48106
- Resolver ID
- CaltechAUTHORS:20140806-133928563
- Created
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2014-08-06Created from EPrint's datestamp field
- Updated
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2019-10-03Created from EPrint's last_modified field
- Caltech groups
- Division of Geological and Planetary Sciences