π¨ Hot off the press πͺ¨ βοΈ Where do you come from, where do you go πΆ fluids that isβ¦ after an earthquake in the dry lower crust? We look into this and more using SEM-CL, EBSD, EMPA, STEM, and FTIR!
Hit the link below π
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2024GC011968
Hit the link below π
https://agupubs.onlinelibrary.wiley.com/doi/full/10.1029/2024GC011968
Comments
(1) Plagioclase in the damage zone of a lower-crustal pseudotachylyte deformed via pulverization-style fragmentation
(2) Liberated H2O as a result of the earthquake remained in grain boundary regions and facilitated neoblast growth and healing of fractures