Home

  • Site Map

    All the web pages on the conference website

Program

Events

Locations

Information

Exhibition

Sponsorships

My Goldschmidt

Role functions

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

Sorry, the PDF cannot be displayed on your browser.

Download abstract

The author has not provided any additional details.

01c: Room 1, Tuesday 23rd June 00:42 - 00:45

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.


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?


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.


Sign in to ask a question.

Goldschmidt® is a registered trademark of the Geochemical Society and of the European Association of Geochemistry

Website managed and hosted by White Iron Conferences on behalf of the international geochemical community