Mantle Plume-Midocean Ridge Interaction: Geophysical Observations and Mantle Dynamics.

We investigate the igneous and mantle dynamic processes of mantle plume midocean ridge interaction with geophysical observational and numerical modeling studies. Bathymetric and gravity anomalies along seafloor isochrons are examined at the Galapagos, Iceland, Azores, Tristan, and Easter plume ridge...

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Bibliographic Details
Main Author: Ito, Garrett T.
Other Authors: MASSACHUSETTS INST OF TECH CAMBRIDGE
Format: Text
Language:English
Published: 1996
Subjects:
Physical and Dynamic Oceanography
Geology
Geochemistry and Mineralogy
*HOT SPOTS
*GEOPHYSICS
*GEOCHEMISTRY
*OCEAN RIDGES
*VOLCANISM
MATHEMATICAL MODELS
INTERACTIONS
FLUX(RATE)
THESES
THREE DIMENSIONAL
BATHYMETRY
MIGRATION
FLOW
PLUMES
VISCOSITY
AZORES
EARTH MANTLE
GRAVITY ANOMALIES
ICELAND
IGNEOUS ROCK
*MID OCEAN RIDGES
Galapagos
Mid-Atlantic Ridge
Tristan
Iceland
Online Access:http://www.dtic.mil/docs/citations/ADA325948
http://oai.dtic.mil/oai/oai?&verb=getRecord&metadataPrefix=html&identifier=ADA325948
Description
Summary:We investigate the igneous and mantle dynamic processes of mantle plume midocean ridge interaction with geophysical observational and numerical modeling studies. Bathymetric and gravity anomalies along seafloor isochrons are examined at the Galapagos, Iceland, Azores, Tristan, and Easter plume ridge systems. Anomaly amplitudes decrease with increasing plume ridge distance whereas along-isochron widths decrease with increasing spreading rate. Three dimensional numerical models predict that along-axis plume width increases with plume volume flux but decreases with increasing spreading rate and plume ridge distance. Ridge migration is predicted to inhibit plume ridge interaction when ridges migrate toward plumes and enhance interaction when ridges migrate away from the plumes. The effects of decompression melting on plume density and viscosity do not appreciably affect the broad scale flow of the plume, but they do contribute significantly to predicted geophysical anomalies. Numerical models predict successfully the geophysical observations at the Iceland-Mid-Atlantic Ridge and Galapagos plume ridge systems. Predictions of geochemistry suggest that mixing between the plumes and ambient mantle most likely occurs below the asthenosphere. Models of the Iceland plume require substantial along-axis melt migration in order to explain a variety of geophysical and geochemical observations.

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