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...
Published in: | Geophysical Journal International |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
Wiley Blackwell Publishing, Inc
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Subjects: | |
Online Access: | http://hdl.handle.net/11336/149019 |