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Can anyone provide me some references regarding development of composite fabric in granitic rocks i.e. where the mesoscopic fabric(magmatic/gneissosity) and magnetic fabric (AMS) fabric are discordant? I am presently working on some Proterozoic and Paleozoic granitoids of Himalaya and there is discrepancy in their field and AMS fabric. This must have been caused by the Tertiary orogeny. Can anyone provide information about similar work from other parts of the world? Best Regards Koushik -- Dr. Koushik Sen Scientist 'B' Wadia Institute of Himalayan Geology Dehra Dun- 248001 India