Changes

==Stratigraphic traps==

==Stratigraphic traps==

Pure [[stratigraphic trap]]s occur where basinal sandstones completely bypassed [[Dip|updip]] areas subsequently filled by mud, providing both top seal and updip lateral seal.<ref name=ch04r22 /><ref name=ch04r36>Galloway, W., E., and T. A. McGilvery, 1995, Facies of a submarine canyon fill reservoir complex, lower Wilcox Group (Paleocene), central Texas coastal plain, in Winn, R., D., Jr., Armentrout, J., M., eds., Turbidites and Associated Deep-Water Facies: WEPM Core Workshop 20, p. 1–23.</ref>

Pure [[stratigraphic trap]]s occur where basinal sandstones completely bypassed [[Dip|updip]] areas subsequently filled by mud, providing both top seal and updip lateral seal.<ref name=ch04r22 /><ref name=ch04r36>Galloway, W. E., and T. A. McGilvery, 1995, Facies of a submarine canyon fill reservoir complex, lower Wilcox Group (Paleocene), central Texas coastal plain, in R. D. Winn, Jr., and J. M. Armentrout, eds., Turbidites and Associated Deep-Water Facies: WEPM Core Workshop 20, p. 1–23.</ref>

==Timing of fault movement==

==Timing of fault movement==