Upper Mantle Structure Along the Axis of the Mid-Atlantic Ridge near Iceland

Apparent velocity measurements of P arrivals from Mid-Atlantic Ridge earthquakes across pairs of stations in Iceland and Greenland have been made using bulletin data. They define both the vertical and horizontal extent of the low velocity anomalous mantle zone between 50° and 70° N.

Bibliographic Details
Published in:Geophysical Journal International
Main Author: Francis, T. J. G.
Format: Text
Language:English
Published: Oxford University Press 1969
Subjects:
Articles
Greenland
Mid-Atlantic Ridge
Iceland
Online Access:http://gji.oxfordjournals.org/cgi/content/short/17/5/507
https://doi.org/10.1111/j.1365-246X.1969.tb00254.x
Description
Summary:Apparent velocity measurements of P arrivals from Mid-Atlantic Ridge earthquakes across pairs of stations in Iceland and Greenland have been made using bulletin data. They define both the vertical and horizontal extent of the low velocity anomalous mantle zone between 50° and 70° N.

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