s made of SIR-B
at Camera (LFC)
the radar data
ly of the same
ndex components
lution: 29.4 m
tion : 17.8 m
rther advantage
can be observed
notographs, in
interpretation .
iring the 17th
take 097.5 on
:nce angle was
contrast with
ata were avail-
ion.
area are the
of the Lower-
(Vail, 1979),
0) as Kashebib
:asionally con-
lated with the
eastern desert
high relief. A
is visible on
ne of the out-
os is slightly
and basic rock
jpwards by the
.sting of meta-
lcanites. They
age with occa-
:inites. Hashad
the basis of
similar rock
is are well re-
jes as a result
' aligned meta-
>r these rocks.
and intricate
The ultramafic
at MSS and LFC
insist of older
thonalites and
.Idly foliated,
le metasedimen-
granitoids are
550 Ma for the
.tic batholiths
unger age (700
i very subdued
(Dixon, 1982).
ind sheets and
ie batholiths.
e on the radar
le MSS and LFC