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Preservation of contrasting geothermal gradients across the Caribbean-North America plate boundary (Motagua Fault, Guatemala)

Abstract : Strike-slip plate boundaries juxtapose crustal blocks that may have different geodynamic origins and therefore different thermal structures. Thermo-kinematic modeling of this type of strike-slip plate boundary predicts an asymmetric signature in the low-temperature thermochronologic record across the fault. Age-elevation profiles of zircon (U-Th)/He ages across the Motagua Fault, a 500km long segment of the transform boundary between the North American and Caribbean plates, document a sharp cooling age discontinuity across the fault. This discontinuity could be interpreted as a difference in denudation history on each side of the fault. However, a low-relief Miocene erosional surface extends across the fault; this surface has been uplifted and incised and provides a geomorphic argument against differential denudation across the fault. By integrating magmatic, volcanic, and heat flow data, age-elevation profiles, and thermo-kinematic modeling, we propose that large horizontal displacement along the Motagua Fault has offset a persistent geothermal asymmetry across the fault and explains both the age discontinuities and the age-elevation patterns. This study illustrates how thermochronology can be used to detect large strike-slip displacements and more generally opens new perspectives in understanding the impact of nonuniform thermal structures on thermochronologic results. Key Points: Effect of geothermal asymmetry on the cooling history of a strike-slip fault Coupled approach of thermochronology, geomorphology and numerical modeling.
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Submitted on : Tuesday, August 20, 2013 - 3:08:31 PM
Last modification on : Tuesday, December 8, 2020 - 10:20:49 AM

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T. Simon-Labric, G. Y. Brocard, C. Teyssier, P.A. van der Beek, M.G. Fellin, et al.. Preservation of contrasting geothermal gradients across the Caribbean-North America plate boundary (Motagua Fault, Guatemala). Tectonics, American Geophysical Union (AGU), 2013, 32, in press. ⟨10.1002/tect.20060⟩. ⟨insu-00852291⟩



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