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Banded Chromite-Fuchsite Quartzite in the Older Supracrustal Sequence of Karnataka


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1 Geological Survey of India, Jayanagar, Bangalore-560011, India
     

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A small enclave of ancient supracrustal rocks (Sargur Group) in Kamataka contains an interesting occurrence of fuchsite quartzite with layers of chromite and other heavy minerals like magnetite, tourmaline, rutile and zircon. The opaque and non-opaque heavy mineral suite is suggestive of a source region rich in sialic components with subordinate ultramafic rocks. This is consistent with the spatial association of these supracrustal rocks with a vast gneissic complex containing numerous enclaves of chromite-rich ultramafic rocks in the vicinity.
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  • Banded Chromite-Fuchsite Quartzite in the Older Supracrustal Sequence of Karnataka

Abstract Views: 194  |  PDF Views: 2

Authors

A. S. Ramiengar
Geological Survey of India, Jayanagar, Bangalore-560011, India
G. R. Devadu
Geological Survey of India, Jayanagar, Bangalore-560011, India
M. N. Viswanatha
Geological Survey of India, Jayanagar, Bangalore-560011, India
N. Chayapathi
Geological Survey of India, Jayanagar, Bangalore-560011, India
M. Ramakrishnan
Geological Survey of India, Jayanagar, Bangalore-560011, India

Abstract


A small enclave of ancient supracrustal rocks (Sargur Group) in Kamataka contains an interesting occurrence of fuchsite quartzite with layers of chromite and other heavy minerals like magnetite, tourmaline, rutile and zircon. The opaque and non-opaque heavy mineral suite is suggestive of a source region rich in sialic components with subordinate ultramafic rocks. This is consistent with the spatial association of these supracrustal rocks with a vast gneissic complex containing numerous enclaves of chromite-rich ultramafic rocks in the vicinity.