Chemical composition and evolution of the garnets in the Astamal Fe-LREE distal skarn deposit, Qara-Dagh–Sabalan metallogenic belt, Lesser Caucasus, NW Iran-Reference-Cited by-同舟云学术

Chemical composition and evolution of the garnets in the Astamal Fe-LREE distal skarn deposit, Qara-Dagh–Sabalan metallogenic belt, Lesser Caucasus, NW Iran

Published:2016-10 Issue: Volume:78 Page:166-175
ISSN:0169-1368
Container-title:Ore Geology Reviews
language:en
Short-container-title:Ore Geology Reviews

Author:

Baghban Saeid,Hosseinzadeh Mohammad Reza,Moayyed Mohsen,Mokhtari Mir Ali Asghar,Gregory Daniel David,Mahmoudi Nia Hosein

Publisher

Elsevier BV

Subject

Economic Geology,Geochemistry and Petrology,Geology

Reference29 articles.

1. Baghban, S., 2013. Genesis, mineralogy, and geochemistry of the Astamal Iron skarn, NE of Kharvana, Eastern Azarbaijan province, Iran. Unpublished M.Sc. thesis, Tabriz University, 185pp. (in Persian with English abstract).

2. Geology, mineral chemistry and formation conditions of calc-silicate minerals of Astamal Fe-LREE distal skarn deposit, Eastern Azarbaijan Province, NW Iran;Baghban;Ore Geol. Rev.,2015

3. Mössbauer study of the thermal behavior of garnets used in high-energy water jet technologies;Barcova;Hyperfine Interact.,2002

4. Compositional zoning and cation diffusion in garnets;Chakraborty,1990

5. Trace element zoning as record of chemical disequilibrium during garnet growth;Chernoff;Geology,1999

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