Articles | Volume 4, issue 1
Earth Surf. Dynam., 4, 71–102, 2016
https://doi.org/10.5194/esurf-4-71-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Special issue: Frontiers in geomorphometry
Research article
21 Jan 2016
Research article
| 21 Jan 2016
Geomorphic analysis of transient landscapes in the Sierra Madre de Chiapas and Maya Mountains (northern Central America): implications for the North American–Caribbean–Cocos plate boundary
L. Andreani and R. Gloaguen
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- Evolution of the Edea‐Eseka geomorphic units: A 'natural laboratory' of a prototype active rifting cross‐cutting the Southern Cameroon (West African) passive margin M. Nsangou et al. 10.1002/gj.3717
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- Climate or tectonics? What controls the spatial-temporal variations in erosion rates across the Eastern Cordillera of Colombia? H. García-Delgado et al. 10.1016/j.gloplacha.2021.103541
2 citations as recorded by crossref.
- Push-pull driving of the Central America Forearc in the context of the Cocos-Caribbean-North America triple junction J. Álvarez-Gómez et al. 10.1038/s41598-019-47617-3
- Seismic hazard at a triple plate junction: the state of Chiapas (México) A. Rodríguez-Lomelí & J. García-Mayordomo 10.1007/s11069-019-03710-4
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Latest update: 09 Aug 2022
Short summary
We use a geomorphic approach in order to unravel the recent tectonic evolution of the Sierra Madre de Chiapas and Maya Mountains (northern Central America). Our results highlight elevated relict landscapes that are characterized by a low-amplitude relief. The distribution of these landscapes results from a tectonic control. We combine our results with published GPS and seismotectonic data in order to extend existing geodynamic models of the North American–Caribbean–Cocos plate boundary.
We use a geomorphic approach in order to unravel the recent tectonic evolution of the Sierra...
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