INVERSION OF SYNTHETIC APERTUR,E R,ADAR (SAR) - MSpace ...

Table 6.2: Con'elation coeffrcielt of the CCRS's airborne ancl the ERS-i
SAR data: Bancl 1 is the airbolne SAR data, ald Bancl 2 is the ERS-I SAR
cl at a.
Table 6.3: Ðigen values and eigen vector.s of trvo components.
t lAelì value Ðigen value (% ) X1 x2
1176.29
58.45
836. i 5
41.55
u.56 0.83
-0.83 0.56
details of the surface geologic features extremely well. All three types of
lineaments in the North Range, rvhich include /y'1[ I4z-tlendilg lineaments,
l{tr4l\4l-tlending lineaments, ancl l{ð-trencling lineaments, are enhancecl as
ale the small structures inside the basin.
The Ratlon transforru analysis are again calriecl out to evaluate the enhancecl
lineaments, and the resulting plot of rnaximurn arnplitucle versus slope
in cleglee is shown in Figure 6.28 (solicl line). The Radon transform analysis
of the oliginal airbolne SAR clata (Figur.e 6.10 (a)) is also plotted (clottecl
line) using the sarle scale to corÌrpa.Ìe rvith that of the PCA irnage. The
plot in Figure 6.28 shorvs the enhauced lineanents in the PCA image (solicl
line) at -16' ancl -26o
comparecl rvith the plot of the or.iginal air.bolne SAR
clata (clotted line). It also shorvs that other chalactelistic ar.nplitucle peaks
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