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In reflection seismology, a dim spot is a local low amplitude seismic attribute anomaly that can indicate the presence of hydrocarbons 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.

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  • Dim spot (en)
  • 地震暗点 (zh)
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  • In reflection seismology, a dim spot is a local low amplitude seismic attribute anomaly that can indicate the presence of hydrocarbons 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. (en)
  • 地震暗点(dim spot)是指地震波屬性在局部顯示的低振幅异常,一般可指碳氢化合物的存在。起因是含碳氢化合物的砂岩其声阻抗比同層含水的声阻抗低的。如果在深層,上層被低声阻抗页岩覆蓋,砂岩頂界反射系数在含碳氢化合物地區會減低。因而造成局部暗点。在淺部地層,页岩和砂岩声阻抗会交叉相反,反而造成亮点(bright spot). (zh)
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  • In reflection seismology, a dim spot is a local low amplitude seismic attribute anomaly that can indicate the presence of hydrocarbons 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. (en)
  • 地震暗点(dim spot)是指地震波屬性在局部顯示的低振幅异常,一般可指碳氢化合物的存在。起因是含碳氢化合物的砂岩其声阻抗比同層含水的声阻抗低的。如果在深層,上層被低声阻抗页岩覆蓋,砂岩頂界反射系数在含碳氢化合物地區會減低。因而造成局部暗点。在淺部地層,页岩和砂岩声阻抗会交叉相反,反而造成亮点(bright spot). (zh)
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