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Tectonics of Monterey Bay
Lead Scientist: Debra Stakes
Project Manager: Dave Caress
Monterey Bay is cross-cut by active faults with low seismicity and
variable mechanisms. The Margin Seismology Program has demonstrated that
small to moderate earthquakes on the Monterey Bay Fault zone (MBFZ) have
nearly pure strike-slip mechanisms and near-vertical dips. The largest
historical earthquakes appear to be on the Monterey Bay fault zone,
including events on Monterey Peninsula. The northern San Gregorio Fault (SGF),
in contrast, while more seismically active, has smaller events with
oblique or thrust mechanisms. The results suggest that the primary strand
of the SGF dips beneath Santa Cruz. The southern SGF zone, which defines
Carmel Canyon and parallels the Big Sur coast, did not show any
significant seismic events during the two years of instrument deployment.
In addition, relocations of historical events do not show any seismic
events for this strand of the SGF. The absence of seismicity could
indicate that the regional strain is being fully accommodated by the
adjacent strands of the MBFZ. Alternatively, this fault segment could be
locked, and building strain until it is released by a large event.
Although the results of the Margin Seismology Project are important and
provocative, the paucity of seismic events suggests that additional
information should be acquired about the three-dimensional structure of
the fault planes and the presence or absence of movement along the
different fault segments. We propose two efforts over the next two years:
1) Add new seismic data to the database when it is acquired during the
continuing development of the MBARI corehole seismometer and LP-1
datalogger. This work would be in
collaboration with Karen McNally, University of California-Santa Cruz.
2) Analyze the newly available marine multichannel seismic reflection
data collected by the US Geological Survey between the Monterey Peninsula and the Golden
Gate in 1990. This effort would be
in collaboration with Steve Lewis, Chief Scientist on the cruise during
which the data were collected as well as the MBARI collaborators, Paull
and Greene.
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