Abstract Details
(2020) Biogeochemical Clues to the Isotopic Mystery of Saratoga Springs
Lollar G, Warr O, Rutledge E & Osburn M
https://doi.org/10.46427/gold2020.1631
The author has not provided any additional details.
14e: Plenary Hall, Wednesday 24th June 00:39 - 00:42
Garnet Lollar
View abstracts at 2 conferences in series
Oliver Warr View all 4 abstracts at Goldschmidt2020
Eric Rutledge
Magdalena Osburn View all 3 abstracts at Goldschmidt2020
Oliver Warr View all 4 abstracts at Goldschmidt2020
Eric Rutledge
Magdalena Osburn View all 3 abstracts at Goldschmidt2020
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 Oliver Warr on Sunday 21st June 19:18
With a crystalline brine-source being reasonably ruled out, I was wondering if you had any thoughts as to the origins of the ionic content/salinity?
With a crystalline brine-source being reasonably ruled out, I was wondering if you had any thoughts as to the origins of the ionic content/salinity?
Submitted by Jennifer McIntosh on Tuesday 23rd June 20:54
Interesting study that should provide important results on fluid and microbial community circulation through crystalline basement rocks. I had a similar question to Oliver's: you mention cation/anion chemistry of springs is distinct from surface waters and shield type brines. Are there any other groundwaters (i.e., potential fluid sources) that have similar major ion chemistries?
Interesting study that should provide important results on fluid and microbial community circulation through crystalline basement rocks. I had a similar question to Oliver's: you mention cation/anion chemistry of springs is distinct from surface waters and shield type brines. Are there any other groundwaters (i.e., potential fluid sources) that have similar major ion chemistries?
Submitted by Jennifer McIntosh on Tuesday 23rd June 20:55
Interesting study that should provide important results on fluid and microbial community circulation through crystalline basement rocks. I had a similar question to Oliver's: you mention cation/anion chemistry of springs is distinct from surface waters and shield type brines. Are there any other groundwaters (i.e., potential fluid sources) that have similar major ion chemistries?
Interesting study that should provide important results on fluid and microbial community circulation through crystalline basement rocks. I had a similar question to Oliver's: you mention cation/anion chemistry of springs is distinct from surface waters and shield type brines. Are there any other groundwaters (i.e., potential fluid sources) that have similar major ion chemistries?
Submitted by Nivea Magalhaes on Tuesday 23rd June 23:17
Can you expand on why the water chemistry (Cation/anion) of Saratoga Springs does not support mixing with a Precambrian crustal brine source?
Can you expand on why the water chemistry (Cation/anion) of Saratoga Springs does not support mixing with a Precambrian crustal brine source?
Submitted by Weibin Chen on Tuesday 23rd June 23:21
Thanks for the nice ppts! It is intriguing to see that linear line above the GMWL! I have two questions: 1. Can you clarify cation/anion data further for source differentiation? So the cation/anion composition between the Saratoga Springs fluids and the Precambrian crustal brine waters are very different (i.e., no mixing scenario is derived)? 2. Are there any sample candidates to fill the gap between the Yellowknife end member and other samples to further strengthen this linear line? Thanks!
Thanks for the nice ppts! It is intriguing to see that linear line above the GMWL! I have two questions: 1. Can you clarify cation/anion data further for source differentiation? So the cation/anion composition between the Saratoga Springs fluids and the Precambrian crustal brine waters are very different (i.e., no mixing scenario is derived)? 2. Are there any sample candidates to fill the gap between the Yellowknife end member and other samples to further strengthen this linear line? Thanks!
Submitted by Weibin Chen on Tuesday 23rd June 23:22
Thanks for the nice ppts! It is intriguing to see that linear line above the GMWL! I have two questions: 1. Can you clarify cation/anion data further for source differentiation? So the cation/anion composition between the Saratoga Springs fluids and the Precambrian crustal brine waters are very different (i.e., no mixing scenario is derived)? 2. Are there any sample candidates to fill the gap between the Yellowknife end member and other samples to further strengthen this linear line? Thanks!
Thanks for the nice ppts! It is intriguing to see that linear line above the GMWL! I have two questions: 1. Can you clarify cation/anion data further for source differentiation? So the cation/anion composition between the Saratoga Springs fluids and the Precambrian crustal brine waters are very different (i.e., no mixing scenario is derived)? 2. Are there any sample candidates to fill the gap between the Yellowknife end member and other samples to further strengthen this linear line? Thanks!
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