SI.DNM,D30.Dep,M.S.BYLEX
.
dralx13X*.C,H
0
a
(CUR.)
CC
I

is
01.1
1

40
0C,H
0
Z2
5

0
6
0
zt
Figure
14.
Scatter
diagram
of
z1
and
z
2
.
(CUR.)
CC
1

15
014
1

40
*C,H
0
a
*
3
6
0
21
Figure
15.
Scatter
diagram
of
z1
and
z3.
and
half
collapse(H)
are
closely
related
to
the
detailed
seismic
intensity(SI),the
depth
to
ter
tiary(Dep),the
subsurface
geology(S)
and
the
microtopograohy(M).
As
shown
in
Figure
15
and
13,total
collapse(C)
is
approximately
similar
to
the
scatter
diagram
of
z
1
and
z
2
,
Moreover,
we
will
report
about
the
principal
component
as
total
term
of
seismic
microzonation
in
future
,in
addition
to
other
term
data,
for
example,
the
ground
vibration,
and
peak
acceleration
etc.
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Akita
University
on
the
Nihonkai
Chubu
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1983
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1985.Site
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Nogoshi,M.
1988.The
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Nihonkai
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1988.Statistical
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1989b.Effect
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geology
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point
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accelerograms
on
the
1983
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Chubu
earthquake.Proc.Nat.Synposium
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&
M.Nakamura
1990.Fundamental
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strongmotion
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on
the
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and
LongPeriod
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N.Nakajima,M.Nogoshi
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23
8
SI.DN11.D50,D0p,1,S.EIMOV.IYINSX',C.H
0
1024