Late Holocene Structural Style and Seismicity of Highly Transpressional Faults in Southern Haiti
The devastating 2010 Haiti earthquake (Mw 7.0) was caused by rupture of the Léogâne, blind, thrust fault located 5 km north of the 1,200‐km‐long, left‐lateral, Enriquillo‐Plantain Garden fault zone (EPGFZ). Unexpectedly, the EPGFZ remained largely quiescent or slightly reactivated during the 2010 ea...
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Veröffentlicht in: | Tectonics (Washington, D.C.) D.C.), 2018-10, Vol.37 (10), p.3834-3852 |
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