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Polyphase Deformation in Phanerozoic Rocks of the Central Himalayan Gneiss, Northwest India: A Discussion

The paper by Powell and Conaghan (1973) gives a detailed account of polyphase deformation and minor structures in the Chandra river valley. We would like to add some additional pertinent data on the structures, tectonic history, and magmatic and metamorphic episodes bearing on the concept of Pretertiary orogenic events in order to discount the suggestion that the central crystalline axis (geanticline) is "fictitious."