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Temporal Patterns of Palaeoflows of Middle and Upper Siwalik Subgroups, Jammu


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1 Department of Geology, University of Jammu, Jammu - 180 004, India
     

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This paper embodies the results of palaeocurrent analysis of two stratigraphic sections exposed at Parmandal-Uttarbani and Papar-Nad, Jammu. The general palaeoflow patterns are due south-southwesteriy with the temporal palaeoflow variations of 40°-183° and 41°-144°for the Middle and Upper Siwalik Subgroups respectively. In the Middle Siwalik Subgroup of Papar-Nad section and Upper Siwalik Subgroup of Parmandal-Uttarbani section, four palaeoflow reversals have been recorded. The temporal palaeoflow patterns and the reversals are related to the tectonic episodicity of the intrabasinal tectonic structures and the basin margin activity.

Keywords

Sedimentology, Palaeocurrents, Siwalik, Jammu, Himalaya.
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  • Temporal Patterns of Palaeoflows of Middle and Upper Siwalik Subgroups, Jammu

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Authors

S. K. Pandita
Department of Geology, University of Jammu, Jammu - 180 004, India
G. M. Bhat
Department of Geology, University of Jammu, Jammu - 180 004, India

Abstract


This paper embodies the results of palaeocurrent analysis of two stratigraphic sections exposed at Parmandal-Uttarbani and Papar-Nad, Jammu. The general palaeoflow patterns are due south-southwesteriy with the temporal palaeoflow variations of 40°-183° and 41°-144°for the Middle and Upper Siwalik Subgroups respectively. In the Middle Siwalik Subgroup of Papar-Nad section and Upper Siwalik Subgroup of Parmandal-Uttarbani section, four palaeoflow reversals have been recorded. The temporal palaeoflow patterns and the reversals are related to the tectonic episodicity of the intrabasinal tectonic structures and the basin margin activity.

Keywords


Sedimentology, Palaeocurrents, Siwalik, Jammu, Himalaya.