Shear zones - an introduction

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  • เผยแพร่เมื่อ 24 ม.ค. 2025

ความคิดเห็น • 11

  • @appliedstratigraphix6844
    @appliedstratigraphix6844 3 ปีที่แล้ว +6

    This is unbelievably good! I wish I had this resource back in college about 20 years ago! You have a gift for breaking down complex ideas, thank you for uploading these.

  • @soroush6788
    @soroush6788 2 ปีที่แล้ว

    Thanks Rob. this video was very useful for me to find out finally how the shear zone is.

    • @robbutler2095
      @robbutler2095  2 ปีที่แล้ว

      thanks - glad you found this useful.

  • @MagmaUpwelling
    @MagmaUpwelling 6 วันที่ผ่านมา

    Hi Rob! Could you please show how to get the animation for the shear zone you showed in this video?

    • @robbutler2095
      @robbutler2095  5 วันที่ผ่านมา

      I made it myself (as all the animations), using illustrator, then putting it in powerpoint and using the fade transition ...

  • @rajinder2662
    @rajinder2662 2 ปีที่แล้ว

    Very good slides.

  • @clezysiki9311
    @clezysiki9311 ปีที่แล้ว

    Thank you so much. Appreciate this

    • @robbutler2095
      @robbutler2095  ปีที่แล้ว

      Glad the channel is useful for you

  • @张宏远-z8t
    @张宏远-z8t 2 ปีที่แล้ว

    I think 45 degrees (αf) may not be always true. The congugate angle 2αf should be random, sometimes 110degrees in middle to lower crust, then less than 90 degrees in most shallow crust, according to quartzofeldspar rocks.

    • @robbutler2095
      @robbutler2095  2 ปีที่แล้ว

      Hi - not so - this is basic geometry for simple shear. Of course rocks can deform in different ways but then it isn't ideal simple shear. There are of course lots of studies - in naturally deformed rocks, in numerical simulations and in theory that deal with general shear - but simple shear (the game for "Ramsay & Graham" shear zone0s is defined as in the video.

    • @张宏远-z8t
      @张宏远-z8t 2 ปีที่แล้ว

      @@robbutler2095 Thanks a lot. Your talk makes me understand that simple shear is the principle mechanism for shear zones of different levels. Maybe what I talk is just in line with a pure shear environment or Anderson model.