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Reflection configuration patterns (view source)
Revision as of 19:19, 29 August 2014
, 19:19, 29 August 2014no edit summary
==Discontinuous reflector patterns==
==Discontinuous reflector patterns==
Five types of discontinuous reflector patterns that help interdepositional systems are shown in [[:file:exploring-for-stratigraphic-traps_fig21-25.png|Figure 2]]. Hummocky strata may be discontinuous point bars and crevasse splays. Chaotic reflectors suggest coarse-grained fluvial or turbidite channel fills. Contorted features may be shale-prone debris flows. Precise identification of depositional environments requires integration with other data.
Five types of discontinuous reflector patterns that help interdepositional systems are shown in [[:file:exploring-for-stratigraphic-traps_fig21-25.png|Figure 2]]. Hummocky strata may be discontinuous point bars and crevasse splays. Chaotic reflectors suggest coarse-grained fluvial or [[turbidite]] channel fills. Contorted features may be shale-prone debris flows. Precise identification of depositional environments requires integration with other data.
[[file:exploring-for-stratigraphic-traps_fig21-26.png|300px|thumb|{{figure number|3}}After .<ref name=ch21r31 />]]
[[file:exploring-for-stratigraphic-traps_fig21-26.png|300px|thumb|{{figure number|3}}After .<ref name=ch21r31 />]]