The sedimentology of the Neoproterozoic Grampian Group and the significance of the Fort William Slide between Spean Bridge and Rubha Cuil-cheanna, Inverness-shire-Reference-Cited by-同舟云学术

The sedimentology of the Neoproterozoic Grampian Group and the significance of the Fort William Slide between Spean Bridge and Rubha Cuil-cheanna, Inverness-shire

Published:1993-05 Issue:1 Volume:29 Page:29-43
ISSN:0036-9276
Container-title:Scottish Journal of Geology
language:en
Short-container-title:Scottish Journal of Geology

Author:

Glover B. W.

Publisher

Geological Society of London

Subject

Geology

Reference55 articles.

1. The Moinian and Dalradian rocks between Glen Ro y and the Monadhliath Mountains, Inverness-shire;ANDERSON;Trans. R. Soc. Edinburgh,1956

2. Tidal-shelf sedimentation: an example from the Scottish Dalradian

3. Dalradian slides and basin development: a radical interpretation of stratigraphy and structure in the SW and Central Highlands of Scotland

4. Recumbent Folds in the Schists of the Scottish Highlands

5. The geology of the neighbourhood of Fort William;BAILEY;Proc. Geol. Assoc. London,1911

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