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- W2596011209 abstract "Pegmatite. aplite and quartz veins of varying dimensions occur in association with pelitic schists, calcareous rocks, quartzites, amphibolites belonging to Ajabgarh Formation, Delhi Group in the Narnaul area and act as important structural markers. The polyphase nature of deformation of the rocks with which these veins occur, is shown by rotation of boudins, presence of overturned tight isoclinal folds resembling F 1 , presence of F 2 folds and refolded folds shown by quartz veins, refolding of limbs of folded pegmatites by folds resembling F 3 . Features like boudins, pinch and swell structures shown by quartz veins and pegmatites at the limbs and along the axial planes of F 1 folds with S 1 development in the host rock and attenuation and disruption of limbs of tight folds resembling F 1 shown by these veins also point to significant amount of flattening during F 1 folding phase and longitudinal stretching in the late stage of their development. Slippage in the later stages of deformation phase (F 3 ) is also distinctly borne dy displaced aplite veins." @default.
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- W2596011209 date "1983-06-01" @default.
- W2596011209 modified "2023-09-25" @default.
- W2596011209 title "Deformation Structures in Pegmatite, Aplite and Quartz Veins in Delhi Group Rocks" @default.
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