Abstract Details
(2020) Ore-Forming Process of the Menez Gwen Hydrothermal Field: In situ S Isotopes and Trace Metals Constraints
Qiu W, Dias ÁA, Costa IMA & Barriga F
https://doi.org/10.46427/gold2020.2143
The author has not provided any additional details.
08m: Room 3, Tuesday 23rd June 22:12 - 22:15
Wenhong Qiu
View all 2 abstracts at Goldschmidt2020
View abstracts at 2 conferences in series
Ágata Alveirinho Dias View all 2 abstracts at Goldschmidt2020 View abstracts at 3 conferences in series
Isabel Maria Amaral Costa View abstracts at 2 conferences in series
Fernando J A S Barriga View all 2 abstracts at Goldschmidt2020 View abstracts at 2 conferences in series
Ágata Alveirinho Dias View all 2 abstracts at Goldschmidt2020 View abstracts at 3 conferences in series
Isabel Maria Amaral Costa View abstracts at 2 conferences in series
Fernando J A S Barriga View all 2 abstracts at Goldschmidt2020 View abstracts at 2 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 22:19
Thank you for the presentation. Can you describe the textures of your pyrite, especially the ones with the very low (approximately -15 per mil) S isotope values? I'm wondering if you have comparable results to the previous presentation (Nozaki) just with fewer analyzed framboids.
Thank you for the presentation. Can you describe the textures of your pyrite, especially the ones with the very low (approximately -15 per mil) S isotope values? I'm wondering if you have comparable results to the previous presentation (Nozaki) just with fewer analyzed framboids.
Submitted by Melissa Anderson on Tuesday 23rd June 19:04
Can you clarify the "subseafloor" nature of these samples? Were they collected by drilling or ROV sampling? At what depths below the seafloor were the samples collected from? Do the chimney samples represent chimney talus?
Can you clarify the "subseafloor" nature of these samples? Were they collected by drilling or ROV sampling? At what depths below the seafloor were the samples collected from? Do the chimney samples represent chimney talus?
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