Geoscience Reference
In-Depth Information
p
M
2
n
X
n
X
n
n
1
1
2
r
1
¼ M
3
M
3
=
2
2
M
1
¼
x
i
;
M
2
¼
ð
x
i
M
1
Þ
;
;
V ¼
100
%;
M
1
i
¼
1
i
¼
1
X
n
2
ð
n
2
Þð
n
3
Þ
;
n
ð
n
1
Þð
n
2
Þ
M
4
M
2
3
ð
n
1
Þ
3
M
3
¼
ð
x
i
M
1
Þ
;
r
2
¼
i¼1
Z
1
X
n
n
ð
n
þ
1
Þ
ð
n
1
Þð
n
2
Þð
n
3
Þ
4
M
4
¼
ð
x
i
M
1
Þ
;
H ¼
f
a
ð
x
Þ
ln f
a
ð
x
Þ
½
dx
;
R
i
¼ x
i
;
max
x
i
;
min
;
i
¼
1
1
M
4
M
2
3
:
M
6
¼
These characteristics and other standard parameters are used to reconstruct f
a
(x).
For instance, if M
3
≈
0, if
a
should be searched for in symmetric distri-
butions. Unit RUA performs this search by selecting continuous distributions from
the knowledge base and estimating their distance from the empirical distribution
using the criterion:
0 and r
1
≈
¼
X
L
2
½
m
i
f
a
ð
x
i
ÞD
x
i
2
v
f
a
ð
x
i
ÞD
x
i
i¼1
The continuous distribution f
*
is chosen to satisfy the following condition:
2
2
ð
f
Þ:
min
f
a
v
ð
f
a
Þ
¼
v
Fig. 3.7 Block scheme of the
data processing in the
sequential analysis procedure
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