Smythe, D.K. , Sowerbutts, W.T.C., Bacon, M. and McQuillin, R. (1972) Deep sedimentary basin below northern Skye and the Little Minch. Nature Physical Science, 236(67), pp. 87-89. (doi: 10.1038/physci236087a0)
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Abstract
The existence of a negative gravity anomaly of amplitude about 20 mgal below northern Skye was first pointed out by Tuson1, who interpreted it as being due to a sedimentary basin bounded at its NE margin by a large NW-SE fault. Our recent geophysical work confirms the existence of this basin, defines its margins more accurately, and provides evidence for the age of the infilling.
| Item Type: | Articles |
|---|---|
| Status: | Published |
| Refereed: | Yes |
| Glasgow Author(s) Enlighten ID: | Smythe, Professor David |
| Authors: | Smythe, D.K., Sowerbutts, W.T.C., Bacon, M., and McQuillin, R. |
| College/School: | College of Science and Engineering > School of Geographical and Earth Sciences |
| Journal Name: | Nature Physical Science |
| Publisher: | Nature Publishing Group |
| ISSN: | 0300-8746 |
| ISSN (Online): | 2058-1106 |
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