Significance of Parting lineation in paleoslope studies: An example from fluvial Siwalik sandstones of Ramnagar-Kaladungi area, Nainital, Uttrakhand
Keywords:
Siwalik Group, Parting lineation, Palaeoslope, Ramnagar-KaladungiAbstract
Parting lineation, a characteristic feature of many fine grained sandstone and siltstone, is widely used as additional parameter to deduce sediment transport direction especially where cross bedding and ripples marks are poorly developed. The Lower and Middle Siwalik Sub Groups of Ramnagar-Kaladungi area exhibit paucity of cross-bedding, though parting lineation are well developed. A sum of 680 measurements of parting lineation from Lower (531) and Middle (149) Siwalik Sub Group are statistically analyzed. Results suggest north-northeast – south-southwest line of sediment transport in the Lower and Middle Siwalik Groups of study area. The deduced line of sediment movement is in conformity with the southerly sediment transport obtained using cross-bedding data in this area and elsewhere in other parts of Siwalik foreland basin. These two-dimensional sedimentary structures may, therefore, provide additional support in deducing palaeoslope.
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