Please use this identifier to cite or link to this item: https://hdl.handle.net/2440/13735
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Type: Journal article
Title: Episodic melt transport at mid-ocean ridges inferred from magnetotelluric sounding
Author: Heinson, G.
Constable, S.
White, A.
Citation: Geophysical Research Letters, 2000; 27(15):2317-2320
Publisher: Amer Geophysical Union
Issue Date: 2000
ISSN: 0094-8276
1944-8007
Abstract: <jats:p>Oceanic crust is generated at mid‐ocean ridges by decompression melting of upwelling mantle at depths of between 50 and 120 km. Geodynamic and geochemical models of upwelling, melt extraction, and melt emplacement into crustal magma reservoirs present a variety of possible migration geometries, most of which assume steady‐state or near steady‐state processes. Here we present results from marine magnetotelluric (MT) measurements, carried out as part of the RAMESSES experiment on the slow spreading Reykjanes Ridge, which support a model of melt extraction and migration that is episodic, rather than steady‐state.</jats:p>
DOI: 10.1029/2000GL011473
Published version: http://dx.doi.org/10.1029/2000gl011473
Appears in Collections:Aurora harvest 7
Environment Institute publications
Geology & Geophysics publications

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