Stable isotope (S, O, H and C) studies of the phyllic and potassic–phyllic alteration zones of the porphyry copper deposit at Sungun, East Azarbaidjan, Iran

Author:

Calagari Ali Asghar

Publisher

Elsevier BV

Subject

Earth-Surface Processes,Geology

Reference24 articles.

1. Calagari, A.A., 1997. Geochemical, stable isotope, noble gas, and fluid inclusion studies of mineralization and alteration at Sungun porphyry copper deposit, East Azarbaidjan, Iran: implication for genesis. Unpublished PhD thesis, University of Manchester, 537 p.

2. Calagari, A.A., Pattrick, R.A.D., Boyce, A.J., Polya, D.A., Fallick, A.E., Burnard, P.G., 1997. Stable isotope studies of the porphyry copper deposit in Sungun, East Azarbaidjan, Iran. Mineral Deposits Studies Group, the Geological Society, Glasgow University, January 8–11, 1997.

3. Veinlets and micro-veinlets studies in Sungun porphyry copper deposit, East Azarbaidjan, Iran;Calagari;Quarterly Journal of Geosciences, Geological Survey of Iran,2001

4. An hydrogen and oxygen isotope study of the San Cristobal mine: implications of the role of water to rock ratio for the genesis of wolframite deposits;Campbell;Economic Geology,1984

5. Direct reduction of sulfates to sulfur dioxide for isotopic analysis;Coleman;Analytical Chemistry,1978

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