Present-day shortening in Southern Haiti from GPS measurements and implications for seismic hazard.

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Bibliographic Details
Title: Present-day shortening in Southern Haiti from GPS measurements and implications for seismic hazard.
Authors: Symithe, Steeve1, Calais, Eric2 eric.calais@ens.fr
Source: Tectonophysics. Jun2016, Vol. 679, p117-124. 8p.
Subjects: Haiti Earthquake, Haiti, 2010, Earthquake hazard analysis, Global Positioning System, Urbanization, Strains & stresses (Mechanics)
Abstract: The ~ 3 M inhabitant capital region of Haiti, severely affected by the devastating January 12, 2010, M7.0 earthquake, continues to expand at a fast rate. Accurate characterization of regional earthquake sources is key to inform urban development and construction practices through improved regional seismic hazard estimates. Here we use a recently updated Global Positioning System (GPS) data set to show that seismogenic strain accumulation in southern Haiti involves an overlooked component of shortening on a south-dipping reverse fault along the southern edge of the Cul-de-Sac basin, in addition to the well-known component of left-lateral strike-slip motion. This tectonic model implies that ground shaking may be twice that expected if the major fault was purely strike-slip, as assumed in the current seismic hazard map for the region. [ABSTRACT FROM AUTHOR]
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Database: Engineering Source
Description
Abstract:The ~ 3 M inhabitant capital region of Haiti, severely affected by the devastating January 12, 2010, M7.0 earthquake, continues to expand at a fast rate. Accurate characterization of regional earthquake sources is key to inform urban development and construction practices through improved regional seismic hazard estimates. Here we use a recently updated Global Positioning System (GPS) data set to show that seismogenic strain accumulation in southern Haiti involves an overlooked component of shortening on a south-dipping reverse fault along the southern edge of the Cul-de-Sac basin, in addition to the well-known component of left-lateral strike-slip motion. This tectonic model implies that ground shaking may be twice that expected if the major fault was purely strike-slip, as assumed in the current seismic hazard map for the region. [ABSTRACT FROM AUTHOR]
ISSN:00401951
DOI:10.1016/j.tecto.2016.04.034