Abstract Details
(2020) Differences in Crustal Ages between the Tula and Scott Mountains of Enderby Land, East Antarctica
Król P, Kusiak MA, Dunkley DJ, Wilde SA, Yi K, Lee S & Whitehouse MJ
https://doi.org/10.46427/gold2020.1369
The author has not provided any additional details.
03e: Room 1, Wednesday 24th June 23:27 - 23:30
Piotr Król
View abstracts at 2 conferences in series
Monika A. Kusiak View all 3 abstracts at Goldschmidt2020 View abstracts at 9 conferences in series
Daniel J. Dunkley View all 2 abstracts at Goldschmidt2020 View abstracts at 9 conferences in series
Simon A. Wilde View all 6 abstracts at Goldschmidt2020 View abstracts at 20 conferences in series
Keewook Yi
Shinae Lee View abstracts at 2 conferences in series
Martin J. Whitehouse View all 12 abstracts at Goldschmidt2020 View abstracts at 17 conferences in series
Monika A. Kusiak View all 3 abstracts at Goldschmidt2020 View abstracts at 9 conferences in series
Daniel J. Dunkley View all 2 abstracts at Goldschmidt2020 View abstracts at 9 conferences in series
Simon A. Wilde View all 6 abstracts at Goldschmidt2020 View abstracts at 20 conferences in series
Keewook Yi
Shinae Lee View abstracts at 2 conferences in series
Martin J. Whitehouse View all 12 abstracts at Goldschmidt2020 View abstracts at 17 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 UQAC Mathieu on Sunday 21st June 15:29
Many thanks for your presentation. I was intrigued by the distinct chemical signatures (HREE-depleted and -undepleted) of your rocks, as something similar is observed in the Abitibi greenstone belt (Mathieu et al. 2020 - https://doi.org/10.3390/min10030242) – would love to discuss the implications of this observation.
Many thanks for you comment, I hope that the presentation has been helpful/useful for you. More details you can find in Król et. a. 2020: 10.1016/j.gr.2019.12.014, but I am open to and keen on any discussion (via email or anywhere here).
Many thanks for your presentation. I was intrigued by the distinct chemical signatures (HREE-depleted and -undepleted) of your rocks, as something similar is observed in the Abitibi greenstone belt (Mathieu et al. 2020 - https://doi.org/10.3390/min10030242) – would love to discuss the implications of this observation.
Many thanks for you comment, I hope that the presentation has been helpful/useful for you. More details you can find in Król et. a. 2020: 10.1016/j.gr.2019.12.014, but I am open to and keen on any discussion (via email or anywhere here).
Submitted by UQAC Mathieu on Sunday 21st June 15:30
Many thanks for your presentation. I was intrigued by the distinct chemical signatures (HREE-depleted and -undepleted) of your rocks, as something similar is observed in the Abitibi greenstone belt (Mathieu et al. 2020 - https://doi.org/10.3390/min10030242) – would love to discuss the implications of this observation.
Many thanks for your presentation. I was intrigued by the distinct chemical signatures (HREE-depleted and -undepleted) of your rocks, as something similar is observed in the Abitibi greenstone belt (Mathieu et al. 2020 - https://doi.org/10.3390/min10030242) – would love to discuss the implications of this observation.
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