HR: 08:15h
AN: T51C-02    [PDF]
TI: Turbidite Based Earthquake Record Along the Northern San Andreas Fault
AU: Morey-Ross, A
EM: morey@coas.oregonstate.edu
AF: College of Oceanic and Atmospheric Sciences, Ocean Admin Bldg. 104 Oregon State University, Corvallis, OR 97331
AU: * Goldfinger, C
EM: gold@coas.oregonstate.edu
AF: College of Oceanic and Atmospheric Sciences, Ocean Admin Bldg. 104 Oregon State University, Corvallis, OR 97331
AU: Nelson, C H
EM: hansnelsonugr@hotmail.com
AF: CSIC/Univ De Granada Inst Andaluz de Ciencias De La Tierra, Campus de Fuentenueva, Granada, 18002 Spain
AU: Chaytor, J
EM: jchaytor@coas.oregonstate.edu
AF: College of Oceanic and Atmospheric Sciences, Ocean Admin Bldg. 104 Oregon State University, Corvallis, OR 97331
AU: Johnson, J E
EM: jjohnson@coas.oregonstate.edu
AF: College of Oceanic and Atmospheric Sciences, Ocean Admin Bldg. 104 Oregon State University, Corvallis, OR 97331
AU: Ericsson, A
AF: College of Oceanic and Atmospheric Sciences, Ocean Admin Bldg. 104 Oregon State University, Corvallis, OR 97331
AB: During June and July, 2002, we collected 60 cores from channel and canyon systems draining the northern California continental margin. The objective of this project is to test the hypothesis that many of the turbidites deposited in these channels result from turbid flows triggered by earthquakes on the northern San Andreas Fault (SAF). Along the northern coast of California between San Francisco and Point Delgada, the San Andreas lies close to the coast or just offshore. No regional stratigraphic datum has yet been found in our cores, however correlation of individual turbidites both along individual channels and across non-connecting channels is robust, providing numerous stratigraphic ties between these systems. We are using Gamma density, high-resolution magnetics, x-ray, and color reflectance data to build a comprehensive regional correlation along the length of the northern San Andreas. That we are able to correlate individual turbidites along channels is not surprising, however correlating turbidites from one channel to another, as much as 300 km away, is surprising. The correlation using patterns in imagery and physical properties suggests that, as we found in Cascadia, many turbid events appear to be recording large earthquakes rather than other possible triggers of these flows. Correlation of events along the margin for large distances suggests an earthquake origin for these turbidites, since other potential triggering mechanisms (except very large storms) operate in only single channels. Such synchronous triggering, only possible with earthquakes, is shown for many events. Channels from separate mineralogic provenances come together at confluences, below which we see either doublets, with no intervening time between them, or bimodal coarse fractions in the turbidites, each peak representing a separate provenance. Perhaps of equal or greater importance, the regional correlation of events implies that the physical property "wiggles" contain information about the earthquakes themselves, since the turbidites located in widely separated and non-communicating channels have, to our knowledge, nothing else in common. Based on initial AMS 14C results, we find that regional correlation is possible for the last ~ 6200 years, and identify 35 events above this datum for the entire region. Of these, 10 events can be correlated along the length of the study region, from the northern limit of the SAF to south of San Francisco. Twelve events correlate along a northern "segment" and nine events correlate along a southern "segment" We find no events that occur clearly in only one channel, and only four events that are found in two and three channels only. These events are in close proximity to the seismically active Mendocino Triple Junction.
DE: 3040 Plate tectonics (8150, 8155, 8157, 8158)
DE: 7221 Paleoseismology
DE: 7223 Seismic hazard assessment and prediction
DE: 7230 Seismicity and seismotectonics
SC: Tectonophysics [T]
MN: 2003 Fall Meeting