Evolution of the Lewisian
This pattern accords with the model, and suggests that the dip changes across the Torridon belt may be due, at least in part, to a strain gradient, and ... Shieldaig peninsula dip gently NE to pass beneath the Diabaig inlier, although they are of comparable strain intensity to those of the Kenmore inlier. ... London263, 383- 385.
| Title | : | Evolution of the Lewisian |
| Author | : | R. Graham Park, John Tarney, Geological Society of London |
| Publisher | : | Blackwell Science Incorporated - 1987 |
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