Physics – Geophysics
Scientific paper
Oct 2002
adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2002georl..29t..34g&link_type=abstract
Geophysical Research Letters, Volume 29, Issue 20, pp. 34-1, CiteID 1973, DOI 10.1029/2002GL015534
Physics
Geophysics
4
Exploration Geophysics: General Or Miscellaneous, Seismology: Paleoseismology, Seismology: Instruments And Techniques, Seismology: General Or Miscellaneous
Scientific paper
To characterize buried portions of the San Andreas Fault (SAF) near its northern extremity in California, three trenches were excavated perpendicular to it and a 3-D georadar data set was acquired. Similar sequences of unconsolidated fluvial sediments, Franciscan serpentinite and active fault zones were observed in the three trenches. Fault traces in the trenches were initially assumed to be part of a single SAF strand. However, the georadar data demonstrated the existence of two SAF strands, one of which was exposed in the central and southern trenches and the other in the northern trench. Offset of a linear-trending georadar feature (possibly a fluvial paleochannel) suggests that 4.5-5.5 m of horizontal displacement occurred across the eastern SAF strand, either during the 1906 San Francisco earthquake or earlier. Georadar reflections from flat-lying and trough-shaped sedimentary boundaries are vertically offset by 0.2-0.3 m along both fault strands.
Baldwin John
Green Alan
Gross Ralf
Holliger Klaus
Horstmeyer Heinrich
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