Changes

==Caveat==

==Caveat==

Faults in most basins are at equilibrium. Those faults that were going to leak have leaked. The present structure and juxtapositions control fault seal behavior and spill points. However, disequilibrium may exist in basins now undergoing rapid migration and fill. The Los Angeles basin (California) is one example. Faults may be dip leaking, but the rate of [[Calculating charge volume|charge]] is greater than the rate of leakage. These faults appear to dip seal—despite seeps along the surface trace of the faults, which indicate dip leakage.

Faults in most basins are at equilibrium. Those faults that were going to leak have leaked. The present structure and juxtapositions control [[fault seal behavior]] and spill points. However, disequilibrium may exist in basins now undergoing rapid migration and fill. The Los Angeles basin (California) is one example. Faults may be dip leaking, but the rate of [[Calculating charge volume|charge]] is greater than the rate of leakage. These faults appear to dip seal—despite seeps along the surface trace of the faults, which indicate dip leakage.

==See also==

==See also==