Deborah S. Kelley coauthored research connecting hydrothermal alteration with motion on a detachment fault at Atlantis Massif. Mineral assemblages and fluid–rock exchange help reconstruct pathways through deforming oceanic material.[ref]
Mass transfer and fluid flow during detachment faulting and development of an oceanic core complex, Atlantis Massif by Chiara Boschi and others. Field and analytical results: alteration, deformation and mass transfer in a detachment system
New to topics? Read the docs here!