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Abstract Details

(2020) Platinum Isotope Variations in Chondrite Meteorites

Hunt A, Iseli L & Schönbächler M

https://doi.org/10.46427/gold2020.1115

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01g: Room 1, Tuesday 23rd June 08:45 - 08:48

Listed below are questions that have been submitted by the community that the author will try and cover in their presentation. To submit a question, ensure you are signed in to the website. Authors or session conveners approve questions before they are displayed here.

Submitted by Mattias Ek on Sunday 21st June 13:28
Do you have an idea of how much of an effect the CRE exposure might have on Pd-Ag or Hf-W ages based on the magnitude of your Pt CRE offsets?
For the most exposed sample measured here, we could expect resolvable differences to nucleosynthetic signatures in the Pd and Ru systems. For Hf-W isochrons, GCR would most likely lead to increased scatter of the data depending on the Ta/W ratios, etc, of the different fractions.

Submitted by Emily Worsham on Monday 22nd June 21:59
Hi Alison, which ordinary chondrite shows the relatively large GCR effect? How well do these data correlate with exposure ages?
The ordinary chondrite with the largest effect is a H5 chondrite, with an average exposure age for H5s. The data correlate well with exposure age, given that the size of the meteoroid and shielding depth are also important.

Submitted by Emily Worsham on Monday 22nd June 22:01
Hi Alison, which ordinary chondrite shows the relatively large GCR effect? How well do these data correlate with exposure ages?


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