The Crustal Structure of Rockall Plateau Microcontinent
Interpretation of seismic refraction measurements and gravity profiles from the Rockall Plateau area of the North-east Atlantic proves that the Plateau is a microcontinent. The depth to the Moho beneath the Plateau varies between 22 and 31 km. P wave velocities of about 6·4 and 7·1 km s−1 were obtai...
Published in: | Geophysical Journal International |
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Format: | Text |
Language: | English |
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Oxford University Press
1972
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Online Access: | http://gji.oxfordjournals.org/cgi/content/short/27/3/259 https://doi.org/10.1111/j.1365-246X.1972.tb06092.x |