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Making regional tectonic maps (view source)
Revision as of 22:13, 3 December 2015
, 22:13, 3 December 2015no edit summary
* Several major structural features
* Several major structural features
The thickest sediments occur over the thin transitional crust, which has subsided beneath the load of more than [[distance::14 km]] (>45,000 ft) of sedimentary rock. (For additional discussion of the structural framework, see Jones and Freed.<ref name=ch04r50>Jones, J. O., and R. L. Freed, eds., 1996, Structural Framework of the Northern Gulf of Mexico: Gulf Coast Association of Geological Sciences, 112 p.</ref>)
The thickest sediments occur over the thin transitional [[crust]], which has subsided beneath the load of more than [[distance::14 km]] (>45,000 ft) of sedimentary rock. (For additional discussion of the structural framework, see Jones and Freed.<ref name=ch04r50>Jones, J. O., and R. L. Freed, eds., 1996, Structural Framework of the Northern Gulf of Mexico: Gulf Coast Association of Geological Sciences, 112 p.</ref>)
==Salt tectonic map==
==Salt tectonic map==