{{Short description|Downward spike in a seismic attribute, often indicative of hydrocarbons}} thumb|The diagram above shows the acoustic impedance relationship that results in a dim spot. In reflection seismology, a '''dim spot''' is a local low-amplitude seismic attribute anomaly that can indicate the presence of hydrocarbons<ref>[https://glossary.slb.com/en/terms/d/dim_spot dim spot], Energy Glossary</ref> and is therefore known as a direct hydrocarbon indicator. It primarily results from the decrease in acoustic impedance contrast when a hydrocarbon (with a low acoustic impedance) replaces the brine-saturated zone (with a high acoustic impedance) that underlies a shale (with the lowest acoustic impedance of the three), decreasing the reflection coefficient.
==Occurrence== For a dim spot to occur, the shale has to have a lower acoustic impedance than both the water sand and the oil/gas sand, which is the opposite situation required for a bright spot to occur. This is possible because compaction causes the acoustic impedances of sands and shales to increase with age and depth but it does not happen uniformly – younger shales have a higher acoustic impedance than younger sands, but this reverses at depth, with older shales having a lower acoustic impedance than older sands.<ref>Brown, Alistar. R., (2010), [https://www.searchanddiscovery.com/documents/2010/40514brown/ "Dim Spots in Seismic Images as Hydrocarbon Indicators", AAPG Search and Discovery Article #40514.]</ref>
Similarly to bright spots, not all dim spots are caused by the presence of hydrocarbons and therefore they should not be treated as conclusive evidence hydrocarbon accumulations.
==See also== *Polarity reversal (seismology)
==References== {{Reflist}} *Hilterman, Fred J., (2001), "Seismic Amplitude Interpretation", SEG.
Category:Seismology
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