Open Access Open Access  Restricted Access Subscription Access
Open Access Open Access Open Access  Restricted Access Restricted Access Subscription Access

Morpho-Chemistry of Rutile in Dengura Manganese Ore Bodies of Koira Valley, Orissa


Affiliations
1 Regional Research Laboratory, Bhubaneswar 751 013, India
2 National Geophysical Research Institute, Hyderabad 500 007, India
3 Department of Geology, Utkal University, Bhubaneswar 751 004, India
     

   Subscribe/Renew Journal


Minute discrete grains of rutile present in manganese ores of Dengura, Koira valley, Sundergarh district, exhibit imperfect columnar and crystallographic forms and an outstanding illustration of twinning. EPMA and EDAX results indicate the presence of Fe, Mn, Cr, Al, Ba, K and Ta, Nb in minor proportion, in rutile crystals. Some of these clements are either present in limited solid solution or later got introduced into its structure during late epigenetic processes. These are detrital grains, pre-existing in the host shale and later affected by solution during epigene manganese are formation.
Subscription Login to verify subscription
User
Notifications
Font Size

Abstract Views: 159

PDF Views: 2




  • Morpho-Chemistry of Rutile in Dengura Manganese Ore Bodies of Koira Valley, Orissa

Abstract Views: 159  |  PDF Views: 2

Authors

B. K. Mohapatra
Regional Research Laboratory, Bhubaneswar 751 013, India
R. Natarajan
National Geophysical Research Institute, Hyderabad 500 007, India
A. K. Paul
Department of Geology, Utkal University, Bhubaneswar 751 004, India
R. K. Sahoo
Regional Research Laboratory, Bhubaneswar 751 013, India

Abstract


Minute discrete grains of rutile present in manganese ores of Dengura, Koira valley, Sundergarh district, exhibit imperfect columnar and crystallographic forms and an outstanding illustration of twinning. EPMA and EDAX results indicate the presence of Fe, Mn, Cr, Al, Ba, K and Ta, Nb in minor proportion, in rutile crystals. Some of these clements are either present in limited solid solution or later got introduced into its structure during late epigenetic processes. These are detrital grains, pre-existing in the host shale and later affected by solution during epigene manganese are formation.