Ridge migration, asthenospheric flow and the origin of magmatic segmentation in the global mid-ocean ridge system

Global observations of mid-ocean ridge (MOR) bathymetry demonstrate an asymmetry in axial depth across ridge offsets that is correlated with the direction of ridge migration. Motivated by these observations, we have developed two-dimensional numerical models of asthenospheric flow and melting beneat...

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מידע ביבליוגרפי
Main Authors: Katz, R, Spiegelman, M, Carbotte, S
פורמט: Journal article
שפה:English
יצא לאור: 2004
תיאור
סיכום:Global observations of mid-ocean ridge (MOR) bathymetry demonstrate an asymmetry in axial depth across ridge offsets that is correlated with the direction of ridge migration. Motivated by these observations, we have developed two-dimensional numerical models of asthenospheric flow and melting beneath a migrating MOR. The modification of the flow pattern produced by ridge migration leads to an asymmetry in melt production rates on either side of the ridge. By coupling a simple parametric model of three dimensional melt focusing to our simulations, we generate predictions of axial depth differences across offsets in the MOR. These predictions are quantitatively consistent with the observed asymmetry. Copyright 2004 by the American Geophysical Union.