Lithospheric structure beneath the northern Central Andean Plateau from the joint inversion of ambient noise and earthquake-generated surface waves
The Central Andean Plateau (CAP), as defined by elevations in excess of 3 km, extends over 1800 km along the active South American Cordilleran margin making it the second largest active orogenic plateau on Earth. The uplift history of this high Plateau, with an average elevation around 4 km above se...
| Main Authors: | , , , , |
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| Other Authors: | |
| Language: | en |
| Published: |
AMER GEOPHYSICAL UNION
2016
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| Online Access: | http://hdl.handle.net/10150/622701 http://arizona.openrepository.com/arizona/handle/10150/622701 |