The Trans-Haitian fault system
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Scientists argue that the deformation has a peculiar chronology involving:
• Initial coupling of the allochthonous terranes during transition from Paleocene epoch to Eocene epoch.
• A development during the Late Miocene epoch when a spaced cleavage was formed within the terrane suture overlapping strata of late Paleocene epoch to late Miocene epoch.
• Diffusion of Pliocene epoch to Pleistocene epoch strike-slip faulting along the traces, reactivating older planes with spaced cleavage.
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Scientists say that basalts within the age range of 0.4 Ma to 1.3 Ma (Ma stands for Mega Anum) were extruded during Pleistocene epoch in the pull-apart basins those were related to N130-trending and N30-normal faults. The N130-trending faults are Septentrional Fault Zone's antagonistic features whereas N30-normal faults are Septentrional Fault Zone's precursory synthetic features.
Open and broad folding and strong uplifts along the NW-striking axes are the part of recent tectonism phase which are very much uniform with the prediction of deformation pattern for EW lateral-left splinter along the boundary of Caribbean-North American tectonic plates.
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