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Geology; November 2002; v. 30; no. 11; p. 1031-1034; DOI: 10.1130/0091-7613(2002)030<1031:EUAADS>2.0.CO;2
© 2002 Geological Society of America
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Epeirogenic uplift above a detached slab in northern Central America

Robert D. Rogers1, Hrafnkell Kárason2 and Robert D. van der Hilst2

1 Department of Geological Sciences and Institute for Geophysics, University of Texas, 4412 Spicewood Springs Road, Building 600, Austin, Texas 78759-8500, USA
2 Department of Earth, Atmospheric, and Planetary Sciences, Massachusetts Institute of Technology, 77 Massachusetts Avenue, 54-918, Cambridge, Massachusetts 02139, USA

P-wave tomographic images reveal that the northern Central America highlands east of the modern volcanic arc overlie a detached slab. Hypsometric analysis of the highlands in Honduras demonstrates that the region is a dissected plateau that is disrupted by normal faults near the North American–Caribbean plate margin. The dissected Central American plateau contains a network of superimposed rivers with meanders cut into bedrock; such a geomorphic character indicates that the regional uplift occurred in the absence of tilting. We propose that the epeirogenic uplift of northern Central America is the buoyant upper-plate response to the influx of mantle asthenosphere following the break-off and sinking of the slab.

Key Words: uplift • slab break-off • Central America • entrenched meanders • tomography




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