CONTRIBUTION TO THE GEOLOGY OF WADI GABGABA : AND ENVIRONS, SOUTH' LA'STERN DESERT, EGYPT.
TAREK MOHAMED KHATER;
Abstract
The geological history of the study area dates back to the
Precambrian, the age of African Shield A significant part of this shield is
seen to the
east of the area studied , manifested in the multicolored,
serrated and high mountains known as the Red Sea Hills Over this shield
at the piedmont of the basement mountains lies a table
land
of highly tilted
Paleozoic
bods
sandstone
sandstone
overlain by nearly horizontal
I
drape .
is due to the westward retreat of this horizontal drape away from the
basement
mountains that
this
the Paleozoic sediments in
remote area
became exposed . In general the sediments make two sinuous belts running
in juxtaposition to the eastern basement mountains
Precambrian, the age of African Shield A significant part of this shield is
seen to the
east of the area studied , manifested in the multicolored,
serrated and high mountains known as the Red Sea Hills Over this shield
at the piedmont of the basement mountains lies a table
land
of highly tilted
Paleozoic
bods
sandstone
sandstone
overlain by nearly horizontal
I
drape .
is due to the westward retreat of this horizontal drape away from the
basement
mountains that
this
the Paleozoic sediments in
remote area
became exposed . In general the sediments make two sinuous belts running
in juxtaposition to the eastern basement mountains
Other data
| Title | CONTRIBUTION TO THE GEOLOGY OF WADI GABGABA : AND ENVIRONS, SOUTH' LA'STERN DESERT, EGYPT. | Other Titles | اضافات جيولوجيه لمنطقه وادى جبجبه وما حولها جنوب الصحراء الشرقيه مصر | Authors | TAREK MOHAMED KHATER | Issue Date | 2004 |
Attached Files
| File | Size | Format | |
|---|---|---|---|
| B18486.pdf | 344.14 kB | Adobe PDF | View/Open |
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