GPS data collected in the Dominican Republic from 1994 to 2001 show that
oblique convergence between the North American and Caribbean plates is parti-tioned
between 5.2+-2 mm/yr of dip-slip reverse motion on the North Hispaniola thrust
(approximately N-S), and 12.8+-2.5 mm/yr and 9.0+-9.0 mm/yr of approximately
E-W left-lateral strike-slip motion on the Septentrional and Enriquillo faults
(95% confidence). The agreement between GPS and paleoseimological slip rates
on the Septentrional fault, together with the 770-960 years since the last
major earthquake and the 800-1200 years maximum repeat time of major earthquakes,
may indicate that the Septentrional fault is currently in the late phase of
its rupture cycle. A fully locked fault accumulating elastic strain at 13
mm/yr implies a current slip deficit of 9.5 m, equivalent to a Mw=7.6-7.8
earthquake if it was entirely released today in a single event. This makes
the Septentrional fault a source of high seismic potential in a densely populated
and rapidly developing area of the Dominican Republic.
|
See also:
Calais, E., Y. Mazabraud, B. Mercier de Lépinay, P. Mann,
P.E. Jansma, and G.S. Mattioli, Oblique collision and strain partitioning
from GPS measurements in the northeastern Caribbean, Geophys. Res. Letters
, in press, 2002.