F. Audemard et al., Trench investigation along the Merida section of the Bocono fault (centralVenezuelan Andes), Venezuela, TECTONOPHYS, 308(1-2), 1999, pp. 1-21
The Bocono fault is a major NE-SW-trending, dextral fault that extends for
about 500 km along the backbone of the Venezuelan Andes. Several large hist
orical earthquakes :in this region have been attributed to the Bocono fault
, surd some of these have been recently associated with specific parts thro
ugh paleoseismologic investigations. A new trench study has been performed,
60 km to the northeast of Merida ill the central Venezuelan Andes, where t
he fault forms a releasing bend, comprising two conspicuous late Holocene f
ault strands that are about 1 km apart. The southern and northern strands c
arry about 70% and 30% (respectively) of the 7-10 mm/yr net slip rate measu
red in this sector, which is based on a 40 vs. 85-100 m right-lateral offse
t of the Late Pleistocene Los Zerpa moraines. A trench excavated on the nor
thern strand of the fault (near Morros de los Hoyos, slightly northeast of
Apartaderos) across a twin shutter ridge and related sag pond exposed two m
ain fault zones cutting Late Pleistocene alluvial and Holocene peat deposit
s. Each zone forms a shutter ridge with peat deposits ponded against the up
lifted block. The paleoearthquake reconstruction derived from this trench a
llows us to propose the occurrence of at least 6-8 earthquakes in the past
9000 yr, yielding a maximum average recurrence interval of about 1100-1500
yr. Based on the northern strands average slip rate (2.6 mm/yr), such an ea
rthquake sequence should have accommodated about 23 m of slip since 9 ka, s
uggesting that the maximum slip per event ranges between 3 and 4 m. No dire
ct evidence for the large 1812 earthquake has been found in the trench, alt
hough this earthquake may have ruptured this section of the fault. Further
paleoseismic studies will investigate the possibility that this event occur
red on the Bocono fault, but ruptured mainly its southern strand in this re
gion. (C) 1999 Elsevier Science B.V. All rights reserved.