Click on figure to see details




|
Figure 5.
Sage
Creek anticline, Fremont County, Wyoming. This well known thrust-fold
structure in the Wind River Basin resulted from Laramide NE-SW directed
compression. Note the location of basement shear zone (red)
to the east of thrust at Dakota level, indicating NE dip as mapped by
well data. This is one of a chain of anticlines 70 miles (105 kms) long
that correlates 100 percent with magnetically mapped basement shear zones.
|