[[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 From Rick Tobin, unpublished data.]]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 From Rick Tobin, unpublished data.]]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.