Slip on this normal fault occurs within the overturned limb of an overturned anticline.
Cambrian strata build the o core part of the anticline, which currently is a flatbottom valley.
His section is located on the other limb of the same anticline as the locality that yielded the species described herein.
The presence of strata susceptible to erosion is responsible for the inversion of the anticline.
Large-scale geometries in the central domain are dominated by an east trending tight anticline which is moderately inclined to the south.
So there is a great zonal area; not a tank, but oil capriciously held in anticline.
It may be a long anticline extending over five or six miles.
There are three mineral beds which are between 2.5 and 8 m thick which are folded in an anticline that plunges to the south-west.
