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Current deformation in Hispaniola from InSAR--derived surface velocities
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Abstract
The oblique convergence between the Caribbean and North American plates is accommodated, in Hispaniola, by left-lateral strike-slip on two major left--lateral fault systems and by intra-arc shortening. We apply a Persistent Scatterer Interferometry (PSInSAR) approach to Sentinel-1 data using six tracks acquired between 2016 and 2023 to generate time series of interseismic velocities over the entire island. We merge the resulting ascending and descending tracks with GNSS--derived velocities to determine a spatially-continuous 3D velocity field that documents deformation gradients across large fault systems. The Enriquillo fault fits a single locked--fault model, while the Septentrional one likely involves several sub--faults. Strain in southeastern Haiti and the southwestern Dominican Republic is well modeled by the J\'er\'emie-Malpasse-Bahoruco oblique reverse fault-system , which represents a significant, but overlooked, regional hazard source.
DOI
https://doi.org/10.31223/X50J32
Subjects
Earth Sciences
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Dates
Published: 2026-05-11 09:52
Last Updated: 2026-05-11 09:52
License
CC-BY Attribution-NonCommercial 4.0 International
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Conflict of interest statement:
None
Data Availability:
https://doi.org/10.5281/zenodo.20094478
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