Changes

==Example of asymmetric dip leakage==

==Example of asymmetric dip leakage==

[[file:evaluating-top-and-fault-seal_fig10-11.png|thumb|{{figure number|2}}After .<ref name=ch10r57>Myers, J., D., 1968, Differential pressures: a trapping mechanism in Gulf Coast oil and gas fields: Gulf Coast Assoc. of Geologists Transactions, vol. 18, p. 56–80.</ref> Copyright: Gulf Coast Assoc. of Geologists.]]

[[file:evaluating-top-and-fault-seal_fig10-11.png|thumb|{{figure number|2}}Chocolate Bayou field, U.S. Gulf Coast, an asymmetric dip leakage.<ref name=ch10r57>Myers, J., D., 1968, Differential pressures: a trapping mechanism in Gulf Coast oil and gas fields: Gulf Coast Assoc. of Geologists Transactions, vol. 18, p. 56–80.</ref> Copyright: Gulf Coast Assoc. of Geologists.]]

An example of asymmetric dip leakage is the Chocolate Bayou field, U.S. Gulf Coast, shown in [[:file:evaluating-top-and-fault-seal_fig10-11.png|Figure 2]]. All of the hanging wall gas accumulations are limited by FPLPs and dip leak. The three gas accumulations in the footwall, however, are all dip sealing; all have gas columns in contact with the fault plane. This pattern of behavior is common in both the U.S. Gulf Coast and the Niger Delta.<ref name=ch10r93 />

An example of asymmetric dip leakage is the Chocolate Bayou field, U.S. Gulf Coast, shown in [[:file:evaluating-top-and-fault-seal_fig10-11.png|Figure 2]]. All of the hanging wall gas accumulations are limited by FPLPs and dip leak. The three gas accumulations in the footwall, however, are all dip sealing; all have gas columns in contact with the fault plane. This pattern of behavior is common in both the U.S. Gulf Coast and the Niger Delta.<ref name=ch10r93 />

==Low-side traps==

==Low-side traps==