4.8 Wills et al. (2000)
1)
Reference
C. J. Wills, M.
Petersen, W. A. Bryant, M. Reichle, G. J. Saucedo, S.
Tan, G.. Taylor, and J. Treiman,
2000, A Site-Conditions Map for California Based on Geology and Shear-wave
Velocity, Bulletin of the Seismological Society of America, 90, No.6B,
S187-S208.
2)
Used
strong motion data
- Area:
- Type pf earthquake:
- Period:
- Number of events:
- Number of records:
- Magnitude:
3)
Formula
for estimation
Will
et al. (2000) have developed a map of site condition in California (1:250000
scale) by grouping geologic units with similar physical properties into
categories that are expected to have similar shear-wave velocity
characteristics Vs30 and composite Vs profiles
for these geologically defined units show that most units do have distinct
shear-wave velocity properties. Of the 556 measured Vs30
values, 411 or 74% fall within the expected range for the unit within which
they are located. The site condition map for
Table 4.8-1
NEHRP-UBC site classification using the average shear-wave velocity to 30 m as
an indicator of site response
Table 4.8-2
Summary of measured Vs30 for statewide map units
Figure 4.8-1
Statewide Vs
classification map
[Category]
B: Plutonic and metamorphic rocks, most
volcanic rocks, coarse sedimentary rocks of
Cretaceous age and older.
BC: Franciscan Complex rocks except “melange” and serpentine, crystalline rocks of the
C:
Franciscan melange and serpentine, sedimentary rocks
of Oligocene to Cetaceous age,
or coarse-grained sedimentary rocks of
younger age.
CD:
Sedimentary rocks of Miocene and younger age, unless formation is notably
coarse
grained, Plio-Pleistocene
alluvial units, older (Pleistocene) alluvium, some areas of
coarse younger alluvium.
D:
Younger (Holocene) alluvium.
DE:
Fill over bay mud in the San Francisco Bay Area, fine-grained alluvial and
estuarine
deposits elsewhere along the coast.
E:
Bay mud and similar intertidal mud.