Changes

==Timing of fault movement==

==Timing of fault movement==

Fault movement timing is critical for trap formation timing. Growth-fault rollover anti-clines develop by updip expansion and sediment entrapment on the downthrown side of the fault and consequent downdip sediment starvation and continued subsidence within the intraslope basin (see Figure 4-43 for geometries above the ''Trim A'' interval along fault A′). Thus, the updip trap for gravity-flow sandstone is the rollover into the fault, formed during the dynamic phase of fault movement.

Fault movement timing is critical for trap formation timing. [[Growth fault|Growth-fault]] rollover anti-clines develop by updip expansion and sediment entrapment on the downthrown side of the fault and consequent downdip sediment starvation and continued subsidence within the intraslope basin (see Figure 4-43 for geometries above the ''Trim A'' interval along fault A′). Thus, the updip trap for gravity-flow sandstone is the rollover into the fault, formed during the dynamic phase of fault movement.

==Fault A′==

==Fault A′==