Abstract Details
(2020) Magmatic Degassing of Trace Elements in Martian Meteorites
Yang S, Humayun M, Irving T, Righter K, Peslier A, Zanda B & Hewins R
https://doi.org/10.46427/gold2020.3001
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01c: Room 1, Tuesday 23rd June 00:42 - 00:45
Shuying Yang
View all 2 abstracts at Goldschmidt2020
View abstracts at 6 conferences in series
Munir Humayan View all 2 abstracts at Goldschmidt2020
Tony Irving
Kevin Righter View abstracts at 14 conferences in series
Anne Peslier View all 2 abstracts at Goldschmidt2020 View abstracts at 18 conferences in series
Brigitte Zanda View abstracts at 14 conferences in series
Roger Hewins View abstracts at 3 conferences in series
Munir Humayan View all 2 abstracts at Goldschmidt2020
Tony Irving
Kevin Righter View abstracts at 14 conferences in series
Anne Peslier View all 2 abstracts at Goldschmidt2020 View abstracts at 18 conferences in series
Brigitte Zanda View abstracts at 14 conferences in series
Roger Hewins View abstracts at 3 conferences in series
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 My Riebe on Sunday 21st June 19:10
Do you know why there is only an effect in Ge? Looking at the enrichment factor plot for terrestrial volcanoes it seems like Ge has an average enrichment factor.
Do you know why there is only an effect in Ge? Looking at the enrichment factor plot for terrestrial volcanoes it seems like Ge has an average enrichment factor.
Submitted by Patricia Clay on Monday 22nd June 14:04
For the bulk meteorite measurements, do you have to worry about loss /modification of more mobile elements due to residence time on Earth's surface?
For the bulk meteorite measurements, do you have to worry about loss /modification of more mobile elements due to residence time on Earth's surface?
Submitted by Tomohiro Usui on Monday 22nd June 23:25
As bulk-rock Mg# of cumulate rocks (nakhlites & chassignites) would not represent melt compositions, I think it seems to be a bit difficult to use Mg# as an indicator of magmatic fractionation of nakhlites & chassignites.
As bulk-rock Mg# of cumulate rocks (nakhlites & chassignites) would not represent melt compositions, I think it seems to be a bit difficult to use Mg# as an indicator of magmatic fractionation of nakhlites & chassignites.
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