Changes

==Fault A′==

==Fault A′==

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Sedimentary-basin-analysis fig4-42.png|{{figure number|3}}Structural elements that define the East Breaks 160-161 minibasin, which is bound on the north by fault A, on the east by faults B and C, and on the south by a salt- cored high. From Armentrout et al. (1991); courtesy Springer-Verlag.

Sedimentary-basin-analysis fig4-42.png|{{figure number|3}}Structural elements that define the East Breaks 160-161 minibasin, which is bound on the north by fault A, on the east by faults B and C, and on the south by a salt- cored high. From Armentrout et al.;<ref>Armentrout, J. M., S. J. Malacek, P. Braithwaite, and C. R. Beeman, 1991, Seismic facies of slope basin turbidite reservoirs, East Breaks 160-161 field: Pliocene–Pleistocene, northwest- ern Gulf of Mexico, in P. Weimer and M. J. Link, eds., Seismic Facies and Sedimentary Processes of Submarine Fans and Turbidite Systems: New York, Springer-Verlag,

Sedimentary-basin-analysis fig4-31.png|{{figure number|4}}Composite chronostratigraphic chart that serves as an age model for the GOM basin Pliocene and Pleistocene, summarizing nine studies published between 1982 and 1993. From Armentrout (1996); courtesy The Geological Society, London.

p. 223–239.</ref> courtesy Springer-Verlag.

Sedimentary-basin-analysis fig4-31.png|{{figure number|4}}Composite chronostratigraphic chart that serves as an age model for the GOM basin Pliocene and Pleistocene, summarizing nine studies published between 1982 and 1993. From Armentrout;<ref>Armentrout, J. M., High-resolution sequence biostratigraphy: examples from the Gulf of Mexico Plio–Pleistocene, in J. Howell and J. Aiken, eds., High Resolution Sequence Stratigraphy: Innovations and Applications: The Geological Society of London Special Publication 104, p. 65–86.</ref> courtesy The Geological Society, London.

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