Sarangi, S., Sarkar, A., Srinivasan, R. and Patel, S.C. (2012) Carbon Isotope Studies of Auriferous Quartz Carbonate Veins from Two Orogenic Gold Deposits from the Neo-Archean Chitradurga Schist Belt, Dharwar Craton, India: Evidence for Mantle: Magmatic Source of Auriferous Fluid. Journal of Asian Earth Sciences, 52, 1-11.
https://doi.org/10.1016/j.jseaes.2012.02.004

has been cited by the following article:

• TITLE: Shear-Controlled Gold Mineralization of G. R. Halli Area of Chitradurga Schist Belt, Dharwar Craton: Insights from Fluid Inclusion Study

  AUTHORS: Govindappa Gopalakrishna, Mohamed Shareef, Poorigali Chowdaiah Nagesh

  KEYWORDS: G. R. Halli, Chitradurga Schist Belt, Dharwar Craton

  JOURNAL NAME: Open Journal of Geology, Vol.8 No.7, July 19, 2018

  ABSTRACT: Gold mineralization at G. R. Halli is located along the Central shear zone of Chitradurga schist belt, extending from west of Gonur, through east of G. R. Halli and C. K. Halli to east of Honnemardi, roughly parallel to stratigraphic units. The NNW-SSE trending shear zone has a width of 0.5 to 1.5 km shows extensive carbonatization of metabasalts and the associated lithologies confined to NNW-WNW trending arcuate brittle-ductile zone. The sheared and silicified contact zones between carbonaceous argillite and schistose metabasalt form the potential sites for localization of mineralization. The gold is associated with sulphides mainly pyrite, arsenopyrite, galena, sphalerite, minor chalcopyrite. Textural relationship indicates two stage sulphide mineral assemblages co-relatable with two stage fluid ascents having temperature of homogenization between 125°C and 256°C. It is a typical epigenetic lode gold system, which got affected by later deformation.