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The great glen fault in the Shetland area

Abstract:

WE apologize to Dr Flinn for any disquiet we may have caused by omitting to refer to his recent paper1. We agree with him that the aeromagnetic map2 distinguishes regions of shallow and deep magnetic basement by the smoothness of the contours. We disagree, however, with his use of the general anomaly level as an indication of sediment thickness, which is the distinction between his pattern A anomalies which "probably overlie deep sedimentary basins" and pattern B which "covers sedimentary bas...

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Publisher copy:
10.1038/227268b0

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Institution:
University of Oxford
Division:
MPLS
Department:
Earth Sciences
Role:
Author
Journal:
Nature More from this journal
Volume:
227
Issue:
5255
Pages:
268-269
Publication date:
1970-01-01
DOI:
ISSN:
0028-0836
Language:
English
Pubs id:
pubs:201549
UUID:
uuid:06633d34-a9bd-473f-9f6c-2d1b8b9c4d4a
Local pid:
pubs:201549
Source identifiers:
201549
Deposit date:
2013-02-20

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