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...

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Published in:Geophysical Journal International
Main Author: Scrutton, R. A.
Format: Text
Language:English
Published: Oxford University Press 1972
Subjects:
Online Access:http://gji.oxfordjournals.org/cgi/content/short/27/3/259
https://doi.org/10.1111/j.1365-246X.1972.tb06092.x
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author Scrutton, R. A.
author_facet Scrutton, R. A.
author_sort Scrutton, R. A.
collection HighWire Press (Stanford University)
container_issue 3
container_start_page 259
container_title Geophysical Journal International
container_volume 27
description 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 obtained for the main crustal layers; these velocities may be typical of microcontinents. The Plateau is approximately in isostatic equilibrium, as too is Rockall Trough. The Trough is underlain by a thin crust, possibly of oceanic origin.
format Text
genre North East Atlantic
genre_facet North East Atlantic
geographic Rockall Plateau
Rockall Trough
geographic_facet Rockall Plateau
Rockall Trough
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op_doi https://doi.org/10.1111/j.1365-246X.1972.tb06092.x
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spelling fthighwire:oai:open-archive.highwire.org:gji:27/3/259 2025-01-16T23:47:06+00:00 The Crustal Structure of Rockall Plateau Microcontinent Scrutton, R. A. 1972-05-01 00:00:00.0 text/html http://gji.oxfordjournals.org/cgi/content/short/27/3/259 https://doi.org/10.1111/j.1365-246X.1972.tb06092.x en eng Oxford University Press http://gji.oxfordjournals.org/cgi/content/short/27/3/259 http://dx.doi.org/10.1111/j.1365-246X.1972.tb06092.x Copyright (C) 1972, Oxford University Press Articles TEXT 1972 fthighwire https://doi.org/10.1111/j.1365-246X.1972.tb06092.x 2012-11-23T22:13:29Z 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 obtained for the main crustal layers; these velocities may be typical of microcontinents. The Plateau is approximately in isostatic equilibrium, as too is Rockall Trough. The Trough is underlain by a thin crust, possibly of oceanic origin. Text North East Atlantic HighWire Press (Stanford University) Rockall Plateau ENVELOPE(-18.833,-18.833,56.333,56.333) Rockall Trough ENVELOPE(-15.036,-15.036,53.825,53.825) Geophysical Journal International 27 3 259 275
spellingShingle Articles
Scrutton, R. A.
The Crustal Structure of Rockall Plateau Microcontinent
title The Crustal Structure of Rockall Plateau Microcontinent
title_full The Crustal Structure of Rockall Plateau Microcontinent
title_fullStr The Crustal Structure of Rockall Plateau Microcontinent
title_full_unstemmed The Crustal Structure of Rockall Plateau Microcontinent
title_short The Crustal Structure of Rockall Plateau Microcontinent
title_sort crustal structure of rockall plateau microcontinent
topic Articles
topic_facet Articles
url http://gji.oxfordjournals.org/cgi/content/short/27/3/259
https://doi.org/10.1111/j.1365-246X.1972.tb06092.x