Mantle flow and melting underneath oblique and ultraslow mid-ocean ridges

Details Mantle flow and melting underneath oblique and ultraslow mid-ocean ridges Mantle flow and melting underneath oblique and ultraslow mid-ocean ridges

Dec 2007

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2007georl..3424307m&link_type=abstract

Geophysical Research Letters, Volume 34, Issue 24, CiteID L24307

Physics

Geophysics

9

Marine Geology And Geophysics: Midocean Ridge Processes, Tectonophysics: Dynamics Of Lithosphere And Mantle: General (1213), Marine Geology And Geophysics: Seafloor Morphology, Geology, And Geophysics, Volcanology: Mid-Oceanic Ridge Processes (1032, 3614), Geochemistry: Magma Genesis And Partial Melting (3619)

Scientific paper

Mid-ocean ridge morphology correlates strongly with spreading rate. As the spreading rate decreases, conductive cooling becomes more important in controlling ridge thermal structure and the axial lithosphere thickens. At ultraslow spreading rates, the ridge axis becomes sufficiently cold that peridotite blocks are emplaced directly at the seafloor and volcanism is limited to localized volcanic centers widely spaced along the ridge axis. Some slow-spreading ridges adopt an ultraslow morphology when their axis is oblique to the spreading direction. We present an analytical solution for mantle flow beneath an oblique ridge and demonstrate that the thermal structure and crustal thickness are controlled by the effective spreading rate (product of the plate separation velocity and the cosine of obliquity). A global compilation of oblique ridges reveals that ultraslow morphology corresponds to effective half rates less than 6.5 mm/yr, resulting in lithosphere that is thicker than ~30 km. We conclude that the transition from slow to ultraslow spreading is not related to a change of melt productivity but rather in the efficiency of vertical melt extraction.

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