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[[file:exploring-for-stratigraphic-traps_fig21-42.png|thumb|300px|{{figure number|1}}Cambrian sandstones in the Lublin Basin (Poland) contain fluorescing oil inclusions trapped before the formation of quartz cements, which degraded the reservoir's quality. From Rick Tobin, unpublished data.]]

[[file:exploring-for-stratigraphic-traps_fig21-42.png|thumb|300px|{{figure number|1}}Cambrian sandstones in the Lublin Basin (Poland) contain fluorescing oil inclusions trapped before the formation of [[quartz]] cements, which degraded the reservoir's quality. From Rick Tobin, unpublished data.]]

==Example: using cementation timing==

==Example: using cementation timing==

In the example shown in [[:file:exploring-for-stratigraphic-traps_fig21-42.png|Figure 1]], [[Cambrian]] sandstones in the Lublin Basin (Poland) contain fluorescing oil inclusions trapped before the formation of quartz cements, which degraded the reservoir's quality. Oil traps could occur [[Dip|updip]] if [[seal]]s were present during the [[migration]] event.

In the example shown in [[:file:exploring-for-stratigraphic-traps_fig21-42.png|Figure 1]], [[Cambrian]] sandstones in the Lublin Basin (Poland) contain fluorescing oil inclusions trapped before the formation of [[quartz]] cements, which degraded the reservoir's quality. Oil traps could occur [[Dip|updip]] if [[seal]]s were present during the [[migration]] event.

==See also==

==See also==