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Shallow Marine Siliciclastic Sedimentation in the Middle Proterozoic Gandikota Formation, Cuddapah Basin, Andhra Pradesh


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1 Geological Survey of India, Project: Cuddapah Basin, Operations: Andhra Pradesh, Bandlaguda, Hyderabad 500 068, India
     

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The Gandikota Formation consists of 40 - 45 m thick shale - siltstone - quartzite (lower member) and 140 - 190 m thick quartzite and siltstone (upper member). Vertical profile of the lower member represents a coarsening up sequence of prograding shoreline setting. As many as eight qualtzite sheets of 15 to 25 m thickness each, constitue the upper member. The herringbone, tabular and trough cross stratified quartzite, and ripple bedded quartzite and siltstone constitute major sedimentary lithofacies in the upper member quartzite sheets. Palaeocurrent mean was towards NW and NNE. A shallow marine environment with poorly contined tidal channels is envisioned for the deposition of the upper member quartzite sheets.

Keywords

Sedimentology, Gandikota Formation, Middle Prolelozoic, Cuddapah Basin, Andhra Pradesh.
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  • Shallow Marine Siliciclastic Sedimentation in the Middle Proterozoic Gandikota Formation, Cuddapah Basin, Andhra Pradesh

Abstract Views: 179  |  PDF Views: 2

Authors

G. Lakshminarayana
Geological Survey of India, Project: Cuddapah Basin, Operations: Andhra Pradesh, Bandlaguda, Hyderabad 500 068, India
S. Bhattacharjee
Geological Survey of India, Project: Cuddapah Basin, Operations: Andhra Pradesh, Bandlaguda, Hyderabad 500 068, India

Abstract


The Gandikota Formation consists of 40 - 45 m thick shale - siltstone - quartzite (lower member) and 140 - 190 m thick quartzite and siltstone (upper member). Vertical profile of the lower member represents a coarsening up sequence of prograding shoreline setting. As many as eight qualtzite sheets of 15 to 25 m thickness each, constitue the upper member. The herringbone, tabular and trough cross stratified quartzite, and ripple bedded quartzite and siltstone constitute major sedimentary lithofacies in the upper member quartzite sheets. Palaeocurrent mean was towards NW and NNE. A shallow marine environment with poorly contined tidal channels is envisioned for the deposition of the upper member quartzite sheets.

Keywords


Sedimentology, Gandikota Formation, Middle Prolelozoic, Cuddapah Basin, Andhra Pradesh.