ion in Togo.
onment in Togo.
Figure 10.
Anticline in Cretaceous sequence north of the Benue River,
Nigeria. X-band radar image, March, 1977; (A) north look,
(B) south look. LANDSAT image, January, 1976; (C) Band 5,
(D) Band 7. Primarily through shadowing, both thin resis-
tant sandstone beds within the core of the structure and the
complex fracture pattern of the southwest end of the structure
are enhanced on the radar image (Gelnett et al., in press).
