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Framboidal – Colloform - Recrystallised Pyrite in the Granitoids of Wahkyn Area, West Khasi Hills, Meghalaya


Affiliations
1 Atomic Minerals Directorate for Exploration and Research, Central Region, Nagpur - 440 013, India
2 Atomic Minerals Directorate for Exploration and Research, Western Region, Jaipur - 302 033, India
3 Atomic Minerals Directorate for Exploration and Research, Southern Region, Bangalore - 560 072, India
     

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Petrographic studies of Proterozoic pyriteferous granitoids forming basement for upper cretaceous Mahadek sediments from Wahkyn area reveal interesting textural peculiarities of Pyrite. These pyrites also reveal interesting structural peculiarities. The three textural pyrite varieties found in the granitoids are: framboidal, colloform and recrystallised which appear both as composite aggregate as well as independent units. Various textures and variation in reflectivity, microhardness and elemental distribution of the pyrites are described. Average Co/Ni ratio along with the textural manifestation of these pyrites attests their sedimentary origin.

Keywords

Ore Mineralogy, Framboidal Pyrite, Radioactive Mineral, Wahkyn, Meghalaya.
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  • Framboidal – Colloform - Recrystallised Pyrite in the Granitoids of Wahkyn Area, West Khasi Hills, Meghalaya

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Authors

N. Ranganath
Atomic Minerals Directorate for Exploration and Research, Central Region, Nagpur - 440 013, India
Ashok Kumar Padhi
Atomic Minerals Directorate for Exploration and Research, Central Region, Nagpur - 440 013, India
Ajoy Kumar Padhi
Atomic Minerals Directorate for Exploration and Research, Western Region, Jaipur - 302 033, India
Ashwini Kumar Rai
Atomic Minerals Directorate for Exploration and Research, Southern Region, Bangalore - 560 072, India

Abstract


Petrographic studies of Proterozoic pyriteferous granitoids forming basement for upper cretaceous Mahadek sediments from Wahkyn area reveal interesting textural peculiarities of Pyrite. These pyrites also reveal interesting structural peculiarities. The three textural pyrite varieties found in the granitoids are: framboidal, colloform and recrystallised which appear both as composite aggregate as well as independent units. Various textures and variation in reflectivity, microhardness and elemental distribution of the pyrites are described. Average Co/Ni ratio along with the textural manifestation of these pyrites attests their sedimentary origin.

Keywords


Ore Mineralogy, Framboidal Pyrite, Radioactive Mineral, Wahkyn, Meghalaya.

References