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On the Occurrence of Sargur Type Banded Iron-Formation in Banded Gneissic Complex of South Rajasthan


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1 Geological Survey of India, Jhalana Dungri, Jaipur, India
     

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The occurrence of BIF from a part of Banded Gneissic Complex of Rajasthan is reported. Older than 3.0 Ga granites, their field-setting and petrochemical characters are comparable to the BIF of older supracrustals of south India (Sargur Group).

Keywords

Banded Iron-Formation, Banded Gneissic Complex, Rajasthan.
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  • On the Occurrence of Sargur Type Banded Iron-Formation in Banded Gneissic Complex of South Rajasthan

Abstract Views: 223  |  PDF Views: 1

Authors

K. C. Sahoo
Geological Survey of India, Jhalana Dungri, Jaipur, India
A. K. Mathur
Geological Survey of India, Jhalana Dungri, Jaipur, India

Abstract


The occurrence of BIF from a part of Banded Gneissic Complex of Rajasthan is reported. Older than 3.0 Ga granites, their field-setting and petrochemical characters are comparable to the BIF of older supracrustals of south India (Sargur Group).

Keywords


Banded Iron-Formation, Banded Gneissic Complex, Rajasthan.