Interpretation
of Continuous-Offset Seismic
Data
in Central
California Margin
Nathaniel E. Putzig, Alan R. Levander
As part of the Pacific Gas & Electric deep crustal geophysical survey, 154 seismic group recorders were deployed in a linear, fixed receiver array to record three one-ton land dynamite shots and 406 10,280-in.3 air gun pops. Receivers were deployed every 350 m in a 50-km line extending to the northeast from the coast at Morro Bay, California. The receivers cross the Sur-Obispo terrane, the Nacimiento and Rinconada fault zones, and part of the sediment-covered Salinian block. A seismic vessel fired the air gun array from 2.4 to 65.5 km offshore at 155-m intervals in line with the onshore receiver spread. The sources extended across the Hosgri fault zone and the Santa Maria basin.
We have produced a reflection image at 5.5 to 6.0 sec two-way traveltime by
CMP stacking traces with offsets less than 20 km. We believe this event, which
is at about 14-km depth and dips landward at 10°-15°, is the top of the lower
crust. An event that appears on common shot and receiver gathers, we interpret
as a wide-angle reflection from the base of this dipping lower crustal layer.
Ray tracing of receiver gather refraction
records indicates that the layer
flattens seaward of the coast. We believe that this feature is a remnant of
oceanic crust that had been subducting beneath the Mesozoic-Cenozoic California
margin and is tectonically correlative with a bright continuous event found on
nearby offshore reflection profiles at about 6 sec two-way traveltime.
AAPG Search and Discovery Article #91035©1988 AAPG-SEPM-SEG Pacific Sections and SPWLA Annual Convention, Santa Barbara, California, 17-19 April 1988.