Mineral chemistry of hydrothermal alteration assemblage in hanging wall Shahapur granite associated with vein-type Gogi uranium deposit, Bhima Basin, Eastern Dharwar Craton, India: Implications for physico-chemical conditions of ore formation

Author:

Raza Mohd Qaim,Absar Nurul

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference130 articles.

1. Hydrothermal epidote – An indicator of temperature and fluid composition;Absar;J. Geol. Soc. India.,1991

2. Petrography, clay mineralogy and geochemistry of clastic sediments of Proterozoic Bhima Group, Eastern Dharwar Craton, India: Implications for provenance and tectonic setting;Absar;J. Appl. Geochem.,2016

3. C, O, Sr and Nd isotope systematics of carbonates of Papaghni sub-basin, Andhra Pradesh, India: Implications for genesis of carbonate-hosted stratiform uranium mineralisation and geodynamic evolution of the Cuddapah basin;Absar;Lithos,2016

4. Absar, N., Raza, M.Q., Ashok, M., Augustine, S., Nizamudheen, B.M., Balakrishnan, S., 2020. Geochronological status of Proterozoic Bhima group, Eastern Dharwar Craton, India; in preparation.

5. Absar, N., Raza, M.Q., Augustine, S., Managave, S., Srinivasa Sarma, D., Balakrishnan, S., 2019. Trace, Rare-Earth Elements and C, O Isotope Systematics of Carbonate Rocks of Proterozoic Bhima Group, Eastern DharwarCraton, India: Implications for the Source of Dissolved Components, Redox Condition and Biogeochemical Cycling of Mesoproterozoic Ocean, in: Mondal, M.E.A. (Ed.), Geological Evolution of the Precambrian Indian Shield. Society of Earth Scientists Series, Springer, pp. 297-326. https://doi.org/10.1007/978-3-319-89698-4_13.

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