Newer Granites of Foyers and Strontian and the Great Glen Fault-Reference-Cited by-同舟云学术

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Newer Granites of Foyers and Strontian and the Great Glen Fault

Published:1967-04 Issue:5084 Volume:214 Page:159-161
ISSN:0028-0836
Container-title:Nature
language:en
Short-container-title:Nature

Author:

MARSTON R. J.

Publisher

Springer Science and Business Media LLC

Subject

Multidisciplinary

Link

http://www.nature.com/articles/214159b0.pdf

Reference10 articles.

1. Kennedy, W. Q., Quart. J. Geol. Soc., 102, 41 (1946).

2. Macgregor, A. G., and Kennedy, W. Q., Sum. Prog. Geol. Survey Gt. Britain for 1931, 105 (1932).

3. Sabine, P. A., Bull. Geol. Survey Gt. Brit., 20, 6 (1963).

4. Munro, M., Scot. J. Geol., 1, 152 (1965).

5. Read, H. H., Liverpool and Manchester Geol. J., 2, 653 (1961).

Cited by 8 articles. 订阅此论文施引文献订阅此论文施引文献，注册后可以免费订阅5篇论文的施引文献，订阅后可以查看论文全部施引文献

1. Reply to Dewey and Ryan Comment on Searle, MP (2021) ‘Tectonic evolution of the Caledonian orogeny in Scotland: a review based on the timing of magmatism, metamorphism and deformation’;Geological Magazine;2022-09-05

2. The metamorphic environment of the Foyers Granitic Complex;Scottish Journal of Geology;1983-11

3. Pattern of Regional Metamorphism suggests a Sinistral Displacement of 160 km along the Great Glen Fault;Nature Physical Science;1973-12

4. Great Glen Fault and Timing of Granite Intrusion on the Proto-Atlantic Continental Margins;Nature Physical Science;1973-08

5. Structures in the south-eastern portion of the Strontian granitic complex, Argyllshire;Scottish Journal of Geology;1973-07

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