Geochemical Data Series: Lesson 5 - Radiogenic isotopes

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  • เผยแพร่เมื่อ 16 พ.ย. 2024

ความคิดเห็น • 10

  • @mainakguha732
    @mainakguha732 2 ปีที่แล้ว +1

    Very helpful; I was reading this from Alan P. Dickin and was not getting anywhere, possibly because I am not from a Geology background and that book is jargon-heavy. Thanks a lot for making this so simple.

  • @Elaaraj-Abdallah
    @Elaaraj-Abdallah ปีที่แล้ว

    Good lessons, thank you for your best explanation.

  • @tiffanyalloyd
    @tiffanyalloyd 2 ปีที่แล้ว

    Thank you! I looked specifically at interpreting the Concordia diagram (U-Pb) and the animations really helped it click for me! :D😀

  • @jsaezf1757
    @jsaezf1757 2 ปีที่แล้ว

    Really well explained!! thanks so muuuuuch!

  • @davenelson413
    @davenelson413 2 ปีที่แล้ว +1

    Thanks, William, with the U-Pb decay @ around 17min 50sec, you were commenting about discordia and the common loss of lead. Where is this lead going to ? decaying to something else or ...... (if you said where, sorry I missed it and couldnt find a reference?) regards, Dave

    • @WillDSmith95
      @WillDSmith95  2 ปีที่แล้ว +1

      Hi Dave - the loss of radiogenic lead is most often ascribed to alteration processes (e.g. interaction with metamorphic, meteoric, or deuteric fluids). The leaching of radiogenic lead is of course problematic as its effects U/Pb values resulting in discordia (I.e. the proportion of U to Pb doesn't honour well defined decay constants!). However, zircon is pretty resistant for the most part... which is why geochronologists prefer it to other geochronometers.

  • @johaneshutabarat683
    @johaneshutabarat683 3 ปีที่แล้ว +1

    thank you very helpful.

  • @gilthunder1737
    @gilthunder1737 3 ปีที่แล้ว +1

    Thnx a lot 🙌✨ was very helpful 🐈🤍

  • @michelleburr45
    @michelleburr45 3 ปีที่แล้ว

    Thank you!

  • @edthoreum7625
    @edthoreum7625 2 ปีที่แล้ว

    5:44 zircons
    6:45 concordia diagram