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GeoRef Categories
Era and Period
Book Series
Date
Availability
oxydravite
Diverse Tourmaline Compositions from Orogenic Gold Deposits in the Hutti-Maski Greenstone Belt, India: Implications for Sources of Ore-Forming Fluids
Crystal structure analyses of four tourmaline specimens from the Cleopatra’s Mines (Egypt) and Jabal Zalm (Saudi Arabia), and the role of Al in the tourmaline group
Al-Fe-Mg ternary diagram of tourmaline coposition. The Ghagri tourmalines p...
Classification diagrams for tourmaline from (A) Hutti and Uti and (B) Hira-...
Ferric-iron-rich tourmaline from the Darasun gold deposit, Transbaikalia, Russia
An Occurrence of Phlogopite-rich Alteration in the Yerington District, Nevada
A rare garnet-tourmaline-sillimanite-biotite-ilmenite-quartz assemblage from the granulite-facies region of south-central Massachusetts
NEW MINERAL NAMES
Trace-element geochemistry of pyrite and arsenopyrite: ore genetic implications for late Archean orogenic gold deposits in southern India
Oxy-vanadium-dravite, NaV 3 (V 4 Mg 2 )(Si 6 O 18 )(BO 3 ) 3 (OH) 3 O: Crystal structure and redefinition of the “vanadium-dravite” tourmaline
Crystal chemistry of povondraite by single-crystal XRD, EMPA, Mössbauer spectroscopy and FTIR
Abstract: The South Kolar Greenstone Belt (SKGB) which is the southern extension of the main Kolar belt hosts several gold deposits and prospects. Among them Chigargunta (CG) and Bisanatham (BN) deposits are most significant deposits. Excluding the western lode of CG which is within the mafic volcanic rocks, majority of the auriferous lodes are hosted in the felsic volcanics (Champion Gneiss) that forms the main eastern mineralization system. In BN, mineralisation is hosted mainly within mafic volcanic rocks that are in closer proximity with Bisanatham granite. Different litho-association has certainly impacted in the development of distinct alteration zones which are mineralogically different in each of these prospects. Three distinct alteration zones with specific mineral assemblages were reported in CG and, at least two zones were identified in BN. The present study focuses on alteration mineralogy and its changes within the alteration zones to characterize the hydrothermal alterations of two distinct gold hosting rocks, in terms of mineralogy and mineral chemistry, in SKGB.