W-Li Potentials in the Tailing Dumps of Rewat Hill, Degana, Rajasthan, NW India; Constraints from Petrography and Geochemistry

Author:

Kumar Suresh,Bhardwaj Shishir,Sharma Achman,Sharma Vivek

Publisher

Springer Science and Business Media LLC

Subject

Geology

Reference28 articles.

1. Anand, S.V., Pandian, M.S., Balakrishnan, S. and Sivasubramaniam, R. (2018) Fluid inclusion, geochemical, Rb–Sr and Sm–Nd isotope studies on tungsten mineralized Degana and Balda granites of the Aravalli craton, NW India. Jour. Earth Syst. Sci., v.127(52), pp.1–20.

2. Auden, J.B. (1941) Report on the wolfram mines on Rewat hill, Degana, Jodhpur State. Geol. Surv. India, Unpbl. Report F.S. 1940–41.

3. Chattopadhyay, B., Chattopadhyay, S. and Bapna, V.S. (1994) Geology and Geochemistry of the Degana Pluton. A Proterozoic Rapakivi Granite in Rajasthan, India. Mineral. Petrol., v.50, pp.69–82.

4. Choudhry A., Gopalan, K., and Sastry, C. A. (1984) Present status of the geochronology of the Precambrian rocks of Rajasthan. Tectonophysics, v.105, pp.131–140.

5. Gao, S., Luo, T.C., Zhang, B.R., Zhang, H.F., Han, Y.W., Zhao, Z.D., Hu, Y.K. (1998) Chemical composition of the continental crust as revealed by studies in East China. Geochim. Cosmochim. Acta, v.62, pp.1959–1975.

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