The effects of small-scale convection in the shallow lithosphere of the North Atlantic

Curie point depth can be used as a proxy for plate temperatures. Data from the North Atlantic (10°-50°N) are used here to determine if the observed oscillations and patterns in Curie depths could be a subproduct of small-scale thermal instabilities arising at the bottom of the lithospheric plates. O...

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Bibliographic Details
Published in:Geophysical Journal International
Main Authors: Likerman, Jeremias, Zlotnik, Sergio, Li, Chun Feng
Format: Article in Journal/Newspaper
Language:English
Published: Wiley Blackwell Publishing, Inc
Subjects:
Online Access:http://hdl.handle.net/11336/149019