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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Main Authors: Katz, R, Spiegelman, M, Carbotte, S
Format: Journal article
Language:English
Published: 2004
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author Katz, R
Spiegelman, M
Carbotte, S
author_facet Katz, R
Spiegelman, M
Carbotte, S
author_sort Katz, R
collection OXFORD
description 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.
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spelling oxford-uuid:299f74d2-eae2-40b7-8dc3-ca7fcc3f65032022-03-26T12:20:13ZRidge migration, asthenospheric flow and the origin of magmatic segmentation in the global mid-ocean ridge systemJournal articlehttp://purl.org/coar/resource_type/c_dcae04bcuuid:299f74d2-eae2-40b7-8dc3-ca7fcc3f6503EnglishSymplectic Elements at Oxford2004Katz, RSpiegelman, MCarbotte, SGlobal 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.
spellingShingle Katz, R
Spiegelman, M
Carbotte, S
Ridge migration, asthenospheric flow and the origin of magmatic segmentation in the global mid-ocean ridge system
title Ridge migration, asthenospheric flow and the origin of magmatic segmentation in the global mid-ocean ridge system
title_full Ridge migration, asthenospheric flow and the origin of magmatic segmentation in the global mid-ocean ridge system
title_fullStr Ridge migration, asthenospheric flow and the origin of magmatic segmentation in the global mid-ocean ridge system
title_full_unstemmed Ridge migration, asthenospheric flow and the origin of magmatic segmentation in the global mid-ocean ridge system
title_short Ridge migration, asthenospheric flow and the origin of magmatic segmentation in the global mid-ocean ridge system
title_sort ridge migration asthenospheric flow and the origin of magmatic segmentation in the global mid ocean ridge system
work_keys_str_mv AT katzr ridgemigrationasthenosphericflowandtheoriginofmagmaticsegmentationintheglobalmidoceanridgesystem
AT spiegelmanm ridgemigrationasthenosphericflowandtheoriginofmagmaticsegmentationintheglobalmidoceanridgesystem
AT carbottes ridgemigrationasthenosphericflowandtheoriginofmagmaticsegmentationintheglobalmidoceanridgesystem