623
3 cmi 4 i I s
Figure 9.-The pattern of radar lineaments density
/in km/km /: i ->2,0j 2 - 2,0rl,5j 3 - 1,5*1,0;
4 - 1,0*0,5; 5 -<0,5.
The satellite lineaments are the continuous lines
which extend 8km in average /maximum i6km/ and looal-
ly fora the longer trends /up to 50km/. The lineaments
of NW-SE /130-150°/ directions, as well as those of
ENE-WSW /70°-80°/ and submeridional /300-10°/ pre
vail.
The first group of lineaments mentioned above
/Nïï-SE orientation/ corresponds to the main structu
ral direction delimited by the edge of the platform
i.e. in this area - by Kock horst anticline and 2y-
rzyn-Abraradw-^widnik horst separated by Stoozek-Doro-
huoza depression /Pig.7,2B/. The seoond group corre
sponds to the directions of the faults /oblique and/or
perpendioular to the Kock horst anticline/, especially
well developed in the platform area adjacent from NE
to this horst.
Basing on the comparison of the remote sensing in
terpretation with two stages of sucoesive geologioal
recognition /Fig.6,7/ it might be stated that the more
Figure 11. Statistical diagrams showing: a -faults in
Meso-Cainozoic sediments, b -faults in Palaeozolo se
diments /state from 1972/, o -faults in Palaeozolo
sediments /state from 1983/, d —Landsat lineaments.
Figure 12. Landsat lineament pattern:! -best visible,
2 -less visible, 3 -weakly visible, 4 -main settle
ments /for comparison only/.
Figure 10. Statistical diagrams of radar lineaments:
a -for the whole area, b -for morainio plateaux, o -
for the area covered with loess, d -for depression
with lake sediments.
oomplete geologioal data - the better ooinoldenoe of
Landsat lineaments and geologioal linear elements
/faults/. It means, therefore, that landsat lineaments
display weak similarity against the earliest fault
pattern interpretation /in the Palaeozolo level/ re
maining however, in a distinot ooinoldenoe with the
further one based on the more detailed geologioal re
cognition of the area. Landsat lineament pattern seems
also to give more information, as it oonoems the di
rection of the faults oblique and perpendicular to the
Kook horst antioline in the area extended towards
north-east.
It is evident that Landsat lineaments display azi
muthal relationship with the faults in Palaeozolo top
/compare also with the statistical diagrams - Fig.lib,
11c and lid/ and might represent their surface pro
jection.
Still comparing remote sensing elements with the
