ments 
elative 
nected 
ted as 
2 b, c) 
e 0 
. Dip- 
>, into 
ke-slip 
logical 
ke-slip 
nclude 
offsets 
T. 
orecast 
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. Visual 
| some 
to the 
iX Step 
, While 
faults. 
btained 
)parent 
amiliar 
yrrelate 
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es and 
is the 
hat the 
assified 
On the 
matrix 
] faults 
id. local 
^ maps 
M low- 
on of 
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stratify 
he zero 
aled on 
rizontal 
1apping 
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and Kv 
its. 
of the 
of the 
nt sea 
mostly 
For the 
btained 
method 
actually works to identify individual faults in regions 
where both topography and tectonic structure are 
complicated. 
The method developed is reproducible. It can improve 
information completeness and impartiality of laboratory 
geological works, contribute to their automation. 
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