Changes

==Fault A′==

==Fault A′==

In the East Breaks 160-161 minibasin, the [[Growth fault|fault]] splay fault A′ forms the northern boundary to the field (Figures 4-42 and 4-43). The dynamic phase of this fault is recorded by the wedge-shaped sediment thickening into the fault, deposited between pre-''Hyal B'' (ca. 1.00 Ma) time of deposition and late ''Trim A'' (ca. 0.56 Ma) time of deposition (Figure 4-31). Its growth phase began about 1.20 Ma.<ref name=ch04r10>Armentrout, J. M., and J. F. Clement, 1990, Biostratigraphic calibration of depositional cycles: a case study in High Island–Galveston–East Breaks areas, offshore Texas: Proceedings, Gulf Coast Section SEPM 11th Annual Research Conference, p. 21–51.</ref><ref name=ch04r7>Armentrout, J. M., 1991, Paleontological constraints on depositional [[modeling]]: examples of integration of biostratigraphy and seismic stratigraphy, Pliocene–Pleistocene, Gulf of Mexico, in P. Weimer, and M. H. Link, eds., Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems: New York, Springer-Verlag, p. 137–170.</ref> Sea-floor expression of this fault clearly indicates offset of Holocene sediments, showing that the fault is currently active (Figure 4-43).

 

In the East Breaks 160-161 minibasin, the [[Growth fault|fault]] splay fault A′ forms the northern boundary to the field ([[:fileSedimentary-basin-analysis fig4-43.png|Figures 2]] and [[:file:Sedimentary-basin-analysis fig4-42.png|3]]). The dynamic phase of this fault is recorded by the wedge-shaped sediment thickening into the fault, deposited between pre-''Hyal B'' (ca. 1.00 Ma) time of deposition and late ''Trim A'' (ca. 0.56 Ma) time of deposition ([[:file:Sedimentary-basin-analysis fig4-31.png|Figure 4]]). Its growth phase began about 1.20 Ma.<ref name=ch04r10>Armentrout, J. M., and J. F. Clement, 1990, Biostratigraphic calibration of depositional cycles: a case study in High Island–Galveston–East Breaks areas, offshore Texas: Proceedings, Gulf Coast Section SEPM 11th Annual Research Conference, p. 21–51.</ref><ref name=ch04r7>Armentrout, J. M., 1991, Paleontological constraints on depositional [[modeling]]: examples of integration of biostratigraphy and seismic stratigraphy, Pliocene–Pleistocene, Gulf of Mexico, in P. Weimer, and M. H. Link, eds., Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems: New York, Springer-Verlag, p. 137–170.</ref> Sea-floor expression of this fault clearly indicates offset of Holocene sediments, showing that the fault is currently active ([[:fileSedimentary-basin-analysis fig4-43.png|Figure 2]]).

==See also==

==See also==