Study of vein-type Cu±Au mineralization in Sangan mineral occurrence (southeastern Torbat-e-Heydarieh), Based on mineralogy, geochemistry and fluid inclusion

Author:

Gholami H,Malekzadeh Shafaroudi A,Karimpour MH, , ,

Publisher

CMV Verlag

Reference41 articles.

1. Geochemistry, geochronology, isotope and fluid inclusion studies of the Kuh-e-Zar deposit, Khaf-Kashmar-Bardaskan magmatic belt, NE Iran: Evidence of gold-rich iron oxide–copper–gold deposit

2. [2] Karimpour M.H., Saadat S., Malekzadeh Shafaroudi A., "Exploration of Cu-Au Iron Oxide and Magnetite Ore Deposits in the VolcanicPlutonic Khaf-Kashmar-Bardsank Belt", 21th National Geosciences conference, Tehran (2003) (In Persian).

3. [3] Mazloumi A.R., Karimpour M.H., Rassa I., Rahimi B., Vosoughi Abedini M., "Kuh-E-Zar Gold Deposit in Torbat-e-Heydaryeh «New Model of Gold Mineralization»", Iranian Journal of Crystallography and Mineralogy 16 (2008) 363- 376 (In Persian).

4. [4] Karimpour M.H., Malekzadeh Shafaroudi A., "Skarn geochemistry - mineralogy and petrology of source rock Sangan Iron mine, Khorasan Razavi, Iran", Scientific Quarterly Journal Geosciences 65 (2008) 108-125 (In Persian).

5. Alteration-mineralization, and radiometric ages of the source pluton at the Sangan iron skarn deposit, northeastern Iran

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