How do detachment faults form at ultraslow mid-ocean ridges in a thick axial lithosphere?
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DOI: 10.1016/j.epsl.2019.116048
Abstract: Abstract Slow-spreading mid-ocean ridges develop large offset normal faults, or detachments, that exhume mantle-derived peridotites to the seafloor. Successive detachments that flip polarity (flip-flop detachments) have been documented in corridors of nearly amagmatic spreading at… read more here.
Keywords: mid ocean; ocean ridges; axial lithosphere; flip flop ... See more keywords