Spatial variations of effective elastic thickness of the lithosphere in Central America and surrounding regions

As a proxy for long-term lithospheric strength, the effective elastic thickness (Te) can be used to understand the relationship between lithospheric rheology and geodynamic evolution of complex tectonic settings. Here we present, for the first time, high-resolution maps of spatial variations of Te i...

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Main Authors: Jiménez-Díaz, Alberto, Ruiz, Javier, Pérez-Gussinyé, Marta, Kirby, Jon, Álvarez-Gómez, Jose, Tejero, Rosa, Capote, Ramon
Format: Journal Article
Published: Elsevier Science BV 2014
Subjects:
Online Access:http://hdl.handle.net/20.500.11937/34235
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author Jiménez-Díaz, Alberto
Ruiz, Javier
Pérez-Gussinyé, Marta
Kirby, Jon
Álvarez-Gómez, Jose
Tejero, Rosa
Capote, Ramon
author_facet Jiménez-Díaz, Alberto
Ruiz, Javier
Pérez-Gussinyé, Marta
Kirby, Jon
Álvarez-Gómez, Jose
Tejero, Rosa
Capote, Ramon
author_sort Jiménez-Díaz, Alberto
building Curtin Institutional Repository
collection Online Access
description As a proxy for long-term lithospheric strength, the effective elastic thickness (Te) can be used to understand the relationship between lithospheric rheology and geodynamic evolution of complex tectonic settings. Here we present, for the first time, high-resolution maps of spatial variations of Te in Central America and surrounding regions from the analysis of the coherence between topography and Bouguer gravity anomaly using multitaper and wavelet methods. Regardless of the technical differences between the two methods, there is a good overall agreement in the spatial variations of Te recovered from both methods. Although absolute Te values can vary in both maps, the qualitative Te structure and location of the main Te gradients are very similar. The pattern of the Te variations in Central America and surrounding regions agrees well with the tectonic provinces in the region, and it is closely related to major tectonic boundaries, where the Middle American and Lesser Antilles subduction zones are characterized by a band of high Te on the downgoing slab seaward of the trenches. These high Te values are related to internal loads (and in the case of the southernmost tip of the Lesser Antilles subduction zone also associated with a large amount of sediments) and should be interpreted with caution. Finally, there is a relatively good correlation, despite some uncertainties, between surface heat flow and our Te results for the study area. These results suggest that although this area is geologically complex, the thermal state of the lithosphere has profound influence on its strength, such that Te is strongly governed by thermal structure.
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publishDate 2014
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spelling curtin-20.500.11937-342352019-02-19T04:27:57Z Spatial variations of effective elastic thickness of the lithosphere in Central America and surrounding regions Jiménez-Díaz, Alberto Ruiz, Javier Pérez-Gussinyé, Marta Kirby, Jon Álvarez-Gómez, Jose Tejero, Rosa Capote, Ramon Caribbean Plate Effective elastic thickness Lithosphere structure Central America Spectral methods As a proxy for long-term lithospheric strength, the effective elastic thickness (Te) can be used to understand the relationship between lithospheric rheology and geodynamic evolution of complex tectonic settings. Here we present, for the first time, high-resolution maps of spatial variations of Te in Central America and surrounding regions from the analysis of the coherence between topography and Bouguer gravity anomaly using multitaper and wavelet methods. Regardless of the technical differences between the two methods, there is a good overall agreement in the spatial variations of Te recovered from both methods. Although absolute Te values can vary in both maps, the qualitative Te structure and location of the main Te gradients are very similar. The pattern of the Te variations in Central America and surrounding regions agrees well with the tectonic provinces in the region, and it is closely related to major tectonic boundaries, where the Middle American and Lesser Antilles subduction zones are characterized by a band of high Te on the downgoing slab seaward of the trenches. These high Te values are related to internal loads (and in the case of the southernmost tip of the Lesser Antilles subduction zone also associated with a large amount of sediments) and should be interpreted with caution. Finally, there is a relatively good correlation, despite some uncertainties, between surface heat flow and our Te results for the study area. These results suggest that although this area is geologically complex, the thermal state of the lithosphere has profound influence on its strength, such that Te is strongly governed by thermal structure. 2014 Journal Article http://hdl.handle.net/20.500.11937/34235 10.1016/j.epsl.2014.01.042 Elsevier Science BV fulltext
spellingShingle Caribbean Plate
Effective elastic thickness
Lithosphere structure
Central America
Spectral methods
Jiménez-Díaz, Alberto
Ruiz, Javier
Pérez-Gussinyé, Marta
Kirby, Jon
Álvarez-Gómez, Jose
Tejero, Rosa
Capote, Ramon
Spatial variations of effective elastic thickness of the lithosphere in Central America and surrounding regions
title Spatial variations of effective elastic thickness of the lithosphere in Central America and surrounding regions
title_full Spatial variations of effective elastic thickness of the lithosphere in Central America and surrounding regions
title_fullStr Spatial variations of effective elastic thickness of the lithosphere in Central America and surrounding regions
title_full_unstemmed Spatial variations of effective elastic thickness of the lithosphere in Central America and surrounding regions
title_short Spatial variations of effective elastic thickness of the lithosphere in Central America and surrounding regions
title_sort spatial variations of effective elastic thickness of the lithosphere in central america and surrounding regions
topic Caribbean Plate
Effective elastic thickness
Lithosphere structure
Central America
Spectral methods
url http://hdl.handle.net/20.500.11937/34235