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Some structural characteristics of the granite of the N.W. Himalayas

✍ Scribed by C.A. McMahon


Book ID
117122005
Publisher
The Geological Society (London)
Year
1896
Tongue
English
Weight
916 KB
Volume
14
Category
Article
ISSN
0016-7878

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This Caledonian pluton exhibits a regular, sub-vertical banding in which layers of dark, relatively fine grained trondhjernite alternate with layers of light, coarse grained granite. The textures and the presence of cross-cutting bands of granite indicate that the light bands were derived by potash