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Oceanic spreading rate and crustal thickness

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Abstract

Examination of oceanic seismic refraction results indicates a correlation between total crustal thickness and spreading rate, with slower spreading producing thinner crust. The effect is seen at spreading rates less than about 20 mm yr−1. The crustal thickness and its dependence on spreading rate are predicted by theoretical modelling of flow and melting beneath mid-ocean ridges.

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Reid, I., Jackson, H.R. Oceanic spreading rate and crustal thickness. Marine Geophysical Researches 5, 165–172 (1981). https://doi.org/10.1007/BF00163477

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