Crossref Citations
This article has been cited by the following publications. This list is generated based on data provided by
Crossref.
Eyles, V. A.
and
MacGregor, A. G.
1952.
The Great Glen Crush-Belt.
Geological Magazine,
Vol. 89,
Issue. 6,
p.
426.
Leedal, Geoffrey Philip
1952.
The Cluanie igneous intrusion, Inverness-Shire And Ross-Shire.
Quarterly Journal of the Geological Society of London,
Vol. 108,
Issue. 1-4,
p.
35.
Anderson, J. G. C.
1956.
II.—The Moinian and Dalradian Rocks between Glen Roy and the Monadhliath Mountains, Inverness-shire.
Transactions of the Royal Society of Edinburgh,
Vol. 63,
Issue. 1,
p.
15.
Watson, Janet
1964.
Conditions in the Metamorphic Caledonides during the Period of Late-orogenic Cooling.
Geological Magazine,
Vol. 101,
Issue. 5,
p.
457.
Munro, M.
1965.
Some structural features of the Caledonian granitic complex at Strontian, Argyllshire.
Scottish Journal of Geology,
Vol. 1,
Issue. 2,
p.
152.
AHMAD, M. U.
1967.
Some Geophysical Observations on the Great Glen Fault.
Nature,
Vol. 213,
Issue. 5073,
p.
275.
Dearnley, R.
1967.
Metamorphism of minor intrusions associated with the Newer Granites of the Western Highlands of Scotland.
Scottish Journal of Geology,
Vol. 3,
Issue. 3,
p.
449.
Holgate, Norman
1969.
Palaeozoic and Tertiary transcurrent movements on the Great Glen fault.
Scottish Journal of Geology,
Vol. 5,
Issue. 2,
p.
97.
Stephenson, D.
1972.
Middle Old Red Sandstone alluvial fan and talus deposits at Foyers, Inverness-shire.
Scottish Journal of Geology,
Vol. 8,
Issue. 2,
p.
121.
Munro, M.
1973.
Structures in the south-eastern portion of the Strontian granitic complex, Argyllshire.
Scottish Journal of Geology,
Vol. 9,
Issue. 2,
p.
99.
WINCHESTER, J. A.
1973.
Pattern of Regional Metamorphism suggests a Sinistral Displacement of 160 km along the Great Glen Fault.
Nature Physical Science,
Vol. 246,
Issue. 154,
p.
81.
Kneen, S. J.
1973.
The Palaeomagnetism of the Foyers Plutonic Complex, Inverness-shire.
Geophysical Journal International,
Vol. 32,
Issue. 1,
p.
53.
Parson, Lindsay M.
1979.
The state of strain adjacent to the Great Glen fault.
Geological Society, London, Special Publications,
Vol. 8,
Issue. 1,
p.
287.
Rock, N. M. S.
1983.
A note on the distribution and significance of metamorphic limestones in the Moine and Lewisian of the Scottish Highlands and Islands.
Geological Magazine,
Vol. 120,
Issue. 6,
p.
639.
Tyler, I. M.
and
Ashworth, J. R.
1983.
The metamorphic environment of the Foyers Granitic Complex.
Scottish Journal of Geology,
Vol. 19,
Issue. 3,
p.
271.
Rock, N. M. S.
Jeffreys, L. A.
and
Macdonald, R.
1984.
The problem of anomalous local limestone-pelite successions within the Moine outcrop; I: metamorphic limestones of the Great Glen area, from Ardgour to Nigg.
Scottish Journal of Geology,
Vol. 20,
Issue. 3,
p.
383.
Garson, M. S.
Coats, J. S.
Rock, N. M. S.
and
Deans, T.
1984.
Fenites, breccia dykes, albitites, and carbonatitic veins near the Great Glen Fault, Inverness, Scotland.
Journal of the Geological Society,
Vol. 141,
Issue. 4,
p.
711.
Torsvik, T.H.
1984.
Palaeomagnetism of the Foyers and Strontian granites, Scotland.
Physics of the Earth and Planetary Interiors,
Vol. 36,
Issue. 2,
p.
163.
Rock, N. M. S.
Macdonald, R.
Szucs, T.
and
Bower, J.
1986.
The comparative geochemistry of some Highland pelites (Anomalous local limestone–pelite successions within the Moine outcrop; II).
Scottish Journal of Geology,
Vol. 22,
Issue. 1,
p.
107.
Storetvedt, K. M.
Tveit, E.
Deutsch, E. R.
and
Murthy, G. S.
1990.
Multicomponent magnetizations in the Foyers Old Red Sandstone (northern Scotland) and their bearing on lateral displacements along the Great Glen Fault.
Geophysical Journal International,
Vol. 102,
Issue. 1,
p.
151.