Abstract Details
(2020) Two-End-Member Mixing in the Fluids Emitted from a Sediment Hosted Geothermal System, Mud Volcano Lei-Gong-Huo, Eastern Taiwan: Evidence from Sr Isotopes
Chao H-C, You C-F & Huang C-C
https://doi.org/10.46427/gold2020.360
The author has not provided any additional details.
14e: Plenary Hall, Wednesday 24th June 00:36 - 00:39
Hung-Chun Chao
View abstracts at 3 conferences in series
Chen-Feng You View all 3 abstracts at Goldschmidt2020
Chun-Chang Huang
Chen-Feng You View all 3 abstracts at Goldschmidt2020
Chun-Chang Huang
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 Chen-Feng You on Friday 19th June 03:44
Great presentation, congratulations! CF
Thanks!
Great presentation, congratulations! CF
Thanks!
Submitted by Drew Syverson on Tuesday 23rd June 21:25
Very interesting talk! I am interested on what processes cause the temporal variation in the fluid sources, sediment versus igneous?
Yeah, they have dipole characteristic except for Zone F MV holes (the most western region) showing residual seawater signal.
Very interesting talk! I am interested on what processes cause the temporal variation in the fluid sources, sediment versus igneous?
Yeah, they have dipole characteristic except for Zone F MV holes (the most western region) showing residual seawater signal.
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