The major, minor and rare earth elements (REE)‍ variations in hydrothermal alteration zones in the volcanic rocks of the west of Naein ophiolite (Central Iran)
The major, minor and rare earth elements (REE)‍ variations in hydrothermal alteration zones in the volcanic rocks of the west of Naein ophiolite (Central Iran)

Neda Tavakoli; Elaheh Namnabat; Moussa Kalimi Noghreyan; Mohammad Ali Mackizadeh

Volume 5, Issue 17 , April 2014, , Pages 137-150

Abstract
  The study area is located 39 km northwest of Naein and is a part of the Urumieh- Dokhtar volcano plutonic arc. The volcanic and pyroclastic rocks have been altered by hydrothermal fluids. ...  Read More
REE geochemistry in skarn garnets from Khut and Panah-Kuh Ore feposit, West of Yazd
REE geochemistry in skarn garnets from Khut and Panah-Kuh Ore feposit, West of Yazd

Azam Zahedi; Mohammad Boomeri; Mohammad Ali Mackizadeh

Volume 4, Issue 13 , April 2013, , Pages 47-66

Abstract
  The Khut and Panah-Kuh skarn deposit is located at about 50 km northwest of Taft in Yazd province. The analyses of major and REE's by microprobe and LA-ICP-MS show that there are two ...  Read More
Skarn mineralization in north part of Kal-e Kafi and its relation with Kal-e Kafi intrusive body
Skarn mineralization in north part of Kal-e Kafi and its relation with Kal-e Kafi intrusive body

Saeideh Ranjbar; Moussa Kalimi Noghreyan; Mohammad Ali Mackizadeh

Volume 3, Issue 9 , June 2012, , Pages 107-126

Abstract
  The Kal-e Kafi granitoid body and related skarn, a part of the Central Iranian zone and the Yazd block, are located 60 Km Northeast of Anarak (Northeast of Isfahan province). This Late ...  Read More
Geology, geochemistry and behavior of rare earth element in the hydrothermal alteration zones, Karkas Mountain North of Isfahan
Geology, geochemistry and behavior of rare earth element in the hydrothermal alteration zones, Karkas Mountain North of Isfahan

Mohammad Ali Mackizadeh; Batoul Taghipour

Volume 2, Issue 8 , January 2012, , Pages 55-68

Abstract
  The Eocene volcanic rocks in the south of Karkas region have been subjected to alteration by hydrothermal and the late magmatic fluids. These volcanics are acidic to intermediate in ...  Read More
Elements variations and the origin of fluids during the hydrothermal alterations in the Astaneh-Arak granitoid
Elements variations and the origin of fluids during the hydrothermal alterations in the Astaneh-Arak granitoid

Rahimeh Mikaili; Moussa Kalimi Noghreyan; Mohammad Ali Mackizadeh; Batoul Taghipour

Volume 2, Issue 7 , June 2011, , Pages 119-134

Abstract
  Seven distinct hydrothermal alteration zones developed within the Astaneh granitoid. The phyllic and silicic alterations have a wide extension in the study area. In the phyllic alteration, ...  Read More
The study of fluid inclusion and mineralogy in the hydrothermal alterations of Astaneh granitoids (Sanandaj_Sirjan zone)
The study of fluid inclusion and mineralogy in the hydrothermal alterations of Astaneh granitoids (Sanandaj_Sirjan zone)

Rahimeh Miekaily; Moussa Kalimi Noghreyan; Mohammad Ali Makki zadeh; Batoul Taghipour; Zahra Tahmasbi

Volume 1, Issue 3 , December 2010, , Pages 89-106

Abstract
  The middle-Jurassic Astaneh granitoid body is composed of mainly of granodiorite. From the ancient time, Au mineralization and prospecting site have been known. The Astaneh granitoid ...  Read More