Abstract Details
(2020) Clumped Isotope Geochemistry of Fe-Carbonates from the Gunflint Formation
Holme E, Henkes G, Rasbury T, Fralick P, Tosca N & Hurowitz J
https://doi.org/10.46427/gold2020.1052
The author has not provided any additional details.
06l: Room 2, Thursday 25th June 00:54 - 00:57
Ella Holme
Gregory Henkes
Troy Rasbury View all 2 abstracts at Goldschmidt2020 View abstracts at 17 conferences in series
Philip Fralick View all 8 abstracts at Goldschmidt2020 View abstracts at 9 conferences in series
Nicholas Tosca View all 2 abstracts at Goldschmidt2020
Joel Hurowitz View all 2 abstracts at Goldschmidt2020 View abstracts at 13 conferences in series
Gregory Henkes
Troy Rasbury View all 2 abstracts at Goldschmidt2020 View abstracts at 17 conferences in series
Philip Fralick View all 8 abstracts at Goldschmidt2020 View abstracts at 9 conferences in series
Nicholas Tosca View all 2 abstracts at Goldschmidt2020
Joel Hurowitz View all 2 abstracts at Goldschmidt2020 View abstracts at 13 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 Daniel Gregory on Thursday 18th June 21:08
Thank you for the great talk. I have two questions, first what did you do to ensure that most / all the calcite and ankerite was gone after the initial acid treatment? Second, you showed that the O and clumped isotopes are consistent with low W/R ratio diagenesis but mention that more work needs to be done to confirm this. What work would you do / are you currently doing?
Thank you for the great talk. I have two questions, first what did you do to ensure that most / all the calcite and ankerite was gone after the initial acid treatment? Second, you showed that the O and clumped isotopes are consistent with low W/R ratio diagenesis but mention that more work needs to be done to confirm this. What work would you do / are you currently doing?
Submitted by Elizabeth Swanner on Monday 22nd June 12:43
I am curious about the implications of the relatively high temperatures from siderite. Does this mean they precipitated from a warm fluid, or can the temperatures associated with later diagenetic or metamorphic events be recorded by clumped isotopes?
I am curious about the implications of the relatively high temperatures from siderite. Does this mean they precipitated from a warm fluid, or can the temperatures associated with later diagenetic or metamorphic events be recorded by clumped isotopes?
Submitted by Chad Wittkop on Monday 22nd June 17:32
Hello, this is very interesting work and I enjoyed hearing about it. Thank you for presenting. Were you able to ensure a complete acid reaction with siderite samples after 60 minutes? And a second question if there is time: Do you know the Mn content of your siderite samples? Thanks again - I look forward to hearing more about your work in the future. cw
Hello, this is very interesting work and I enjoyed hearing about it. Thank you for presenting. Were you able to ensure a complete acid reaction with siderite samples after 60 minutes? And a second question if there is time: Do you know the Mn content of your siderite samples? Thanks again - I look forward to hearing more about your work in the future. cw
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