Abstract Details
(2020) Uranium Isotopes Constrain Sediment Transport Times to the Bengal Fan
Clinger A, DePaolo D & Christensen J
https://doi.org/10.46427/gold2020.452
The author has not provided any additional details.
10f: Plenary Hall, Thursday 25th June 23:15 - 23:18
Anna Clinger
View abstracts at 4 conferences in series
Donald J. DePaolo View all 6 abstracts at Goldschmidt2020 View abstracts at 20 conferences in series
John Christensen View all 2 abstracts at Goldschmidt2020 View abstracts at 3 conferences in series
Donald J. DePaolo View all 6 abstracts at Goldschmidt2020 View abstracts at 20 conferences in series
John Christensen View all 2 abstracts at Goldschmidt2020 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 Sarah Feakins on Thursday 25th June 01:34
Hi Anna, would you expect longer transit times during the Miocene and Pliocene, sediments being supplied to the Bengal Fan, like the interglacials? thanks, Sarah Feakins
Hi Anna, would you expect longer transit times during the Miocene and Pliocene, sediments being supplied to the Bengal Fan, like the interglacials? thanks, Sarah Feakins
Submitted by Marisa Repasch on Thursday 25th June 17:34
Hi Anna, thanks for sharing your cool U-series dataset. I have a few questions for you: 1) How do you quantify the amount of 234U lost to recoil? How does this affect your comminution age estimates? 2) Why do you think the comminution ages are so short in MIS7? 3) How much comminution can occur in the marine setting? Is there any exchange with U-series isotopes in seawater (I guess authigenic U) that would affect your ages? Thanks!
Hi Anna, thanks for sharing your cool U-series dataset. I have a few questions for you: 1) How do you quantify the amount of 234U lost to recoil? How does this affect your comminution age estimates? 2) Why do you think the comminution ages are so short in MIS7? 3) How much comminution can occur in the marine setting? Is there any exchange with U-series isotopes in seawater (I guess authigenic U) that would affect your ages? Thanks!
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