%0 Journal Article
%T El sismo del 21/12/2001 en los Andes Meride£¿os
%A Rengifo
%A Mart¨ªn
%A Laffaille
%A Jaime
%A Choy
%A Jos¨¦
%J Revista de la Facultad de Ingenier¨ªa Universidad Central de Venezuela
%D 2010
%I Scientific Electronic Library Online
%X on december 21, 2001, at nearly five o¡äclock in the afternoon, a strong earthquake shook a large extent of the venezuelan andes. this event was reported by the laboratorio de geof¨ªsica (universidad de los andes) with magnitude mb = 5,7; epicentral coordinates at 8.23o n - 70.96o w (northeast of aricagua, m¨¦rida state) and 6 km depth. the focal mechanism was determined using 33 p-wave first motion polarities. the solution is given by: (a) strike = 228o, dip = 75o and slip = 137o; (b) strike = 328o, dip = 48o and slip = 137o. the distribution of aftershocks shows that (a) is the fault plane, indicating a right lateral strike slip faulting. due to the location of its epicenter, its type of faulting and the distribution of its aftershocks, it is considered that this event broke the caparo fault, venezuela. another set of events occurred on the 26th of the same month, at approximately 20 km to the southwest. they also were associated with the caparo fault, and produced a set of polarities consistent with the focal mechanism of the main event of december the 21th. initially, no serious damages were reported, but a few weeks later it was known that they occurred in the el quin¨®, a village of difficult access for its geographical location. the collected macroseismic information was enough to make an isosistic map, whose curves show some elongation with a ne-sw trend. determination of earthquake parameters from this map point out the feasibility of the application, with good results, of the shebalin seismic-field equations to historical earthquakes occurring in the venezuelan andes
%K earthquake
%K intensity
%K vulnerability
%K caparo fault
%K seismicity.
%U http://www.scielo.org.ve/scielo.php?script=sci_abstract&pid=S0798-40652010000100001&lng=en&nrm=iso&tlng=en