| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 7699753 | Marine Chemistry | 2012 | 11 Pages |
Abstract
⺠Large Br/Cl changes in vent fluids have occurred at Milos in contrast to MOR systems. ⺠Halite contributes the Br/Cl changes in segregated vapors as pore pressure varied. ⺠Continuously boiling off the vapors induces residual brines has low Br/Cl at deep. ⺠High I/Cl in cave and brine fluids imply sediment contribution have occurred at deep. ⺠The I/Cl in brines and cave fluids fall in a similar range as those in MOR systems.
Related Topics
Physical Sciences and Engineering
Chemistry
Chemistry (General)
Authors
Shein-Fu Wu, Chen-Feng You, Eugenia Valsami-Jones, Emmanuel Baltatzis, Min-Lin Shen,