10,351
edits
Changes
Jump to navigation
Jump to search
Line 20:
Line 20: − +
Identifying depositional sequences in seismic sections (view source)
Revision as of 19:47, 28 July 2014
, 19:47, 28 July 2014→GOM basin example
==GOM basin example==
==GOM basin example==
[[file:sedimentary-basin-analysis_fig4-19.png|thumb|300px|{{figure number|1}}Seismic reflection profile from the East Breaks field area. Modified. Copyright: Armentrout (1993); courtesy Gulf Coast SEPM.]]
[[file:sedimentary-basin-analysis_fig4-19.png|thumb|300px|{{figure number|1}}Seismic reflection profile from the East Breaks field area. Modified. Copyright: Armentrout;<ref name=Armentrout1993>Armentrout, J. M., 1993, Relative seal-level variations and fault-salt response: offshore Texas examples: Proceedings, Gulf Coast Section SEPM 14th Annual Research Conference, p. 1–7.</ref> courtesy Gulf Coast SEPM.]]
In the shelf-margin facies of the East Breaks study area of the GOM basin, a depositional sequence in its simplest form is identified in seismic sections as a couplet consisting of two patterns:
In the shelf-margin facies of the East Breaks study area of the GOM basin, a depositional sequence in its simplest form is identified in seismic sections as a couplet consisting of two patterns: