Interpreting a seismic reflection profile - Inner Moray Firth

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  • เผยแพร่เมื่อ 25 ก.ค. 2024
  • Part of the Shear Zone channel. This is an introduction to interpreting a seismic reflection profile - using an example from the Inner Moray Firth.

ความคิดเห็น • 7

  • @olaal-najjar7391
    @olaal-najjar7391 ปีที่แล้ว

    This was really helpful. Thank you

  • @SudipRay1983
    @SudipRay1983 ปีที่แล้ว

    Awesome explanation.

    • @robbutler2095
      @robbutler2095  ปีที่แล้ว

      thanks - glad you found it useful!

  • @tomonslow4267
    @tomonslow4267 2 ปีที่แล้ว

    how could you check for 'Normal polarity' for sea-bed relectors for eurropean polarity conventions ? Thank you :)

    • @robbutler2095
      @robbutler2095  2 ปีที่แล้ว +1

      Hi Tom - thanks for the question. There are competing ways of displaying polarity, generally referred to as "American" and "European" ... in practice, opposite to each other. But actually a greater issue is the choice of colour bar issued to display the image... so rules like "blue = hard kick" is not reliable, regardless of the origin of the image. So a good check with marine data is to look at the seabed - which should of course reflect a positive impedance contrast (as sediment/rock have higher velocities than seawater). For onshore data this is much tougher... For more (technical) info - check out SEGwiki.... as a good starting point....

  • @haroonshaikh9771
    @haroonshaikh9771 10 หลายเดือนก่อน

    7:18 Is it possible to identify more than one reactivation phases of a fault from a seismic profile?

    • @robbutler2095
      @robbutler2095  10 หลายเดือนก่อน

      Yes - if the growth strata are resolvable...