Geoscience Reference
In-Depth Information
or
(
Γ
+
Γ
T
)
/
2=
M
+
ΩΩ
,
(7-59)
which concludes our proof.
Since we have determined
˙
Ω
in (7-57), we can get
Ω
by integration:
Ω
(
t
)=
Ω
(
t
0
)+
t
t
0
˙
Ω
dt ,
(7-60)
where the initial orientation
Ω
(
t
0
) is obtained from the star trackers. Squar-
ing the result for
Ω
(
t
) yields
ΩΩ
, which is needed in (7-59) so that we
find
M
=(
Γ
+
Γ
T
)
/
2
−
ΩΩ
(7-61)
as final result for the desired Marussi tensor
M
. Many more details may be
found in Rummel (1986).