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Line 17: − Access to core, samples, and modern wireline log suites greatly facilitates subsurface interpretation. In the example below, both lateral and top seals in the dolomite reservoir were created by anhydrite cementation during early diagenesis. Primary fades changes do not control the location of the trap. − + + +
Diagenetic impact on traps (view source)
Revision as of 19:50, 22 January 2014
, 19:50, 22 January 2014no edit summary
==Example==
==Example==
[[file:exploring-for-stratigraphic-traps_fig21-5.png|thumb|{{figure number|21-5}}From unpublished data by R.C. Tobin, 1987.]]
[[file:exploring-for-stratigraphic-traps_fig21-5.png|thumb|{{figure number|1}}From unpublished data by R.C. Tobin, 1987.]]
Access to core, samples, and modern wireline log suites greatly facilitates subsurface interpretation. In [[:file:exploring-for-stratigraphic-traps_fig21-5.png|Figure 1]], both lateral and top seals in the dolomite reservoir were created by anhydrite cementation during early diagenesis. Primary fades changes do not control the location of the trap.
==See also==
==See also==