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Spear, F. (2005) Metamorphic Phase Equilibria and Pressure-Temperature-Time Paths. Department of Earth and Environmental Sciences Rensselaer, Polytechnic Institute Troy, New York, Mineralogical Society of America, Washington DC.

has been cited by the following article:

• TITLE: Geochemistry, Mineral Chemistry and Thermobarometry of Boneh-Shorou Amphibolites in Gelmandeh Massive (Saghand-Central Iran)

  AUTHORS: Arash Gourabjeiri-Pour, Soraya Heuss-Aßbichler, Mohsen Mobasheri, Parivash Mahdavi

  KEYWORDS: Amphibolite, Mineral Chemistry, Thermobarometry, Gelmandeh Massive, Boneh-Shorou, Central Iran

  JOURNAL NAME: Open Journal of Geology, Vol.6 No.8, August 18, 2016

  ABSTRACT: The Gelmandeh Massive is located in the Central part of Iranian Microcontinent. Amphibolitic rocks occupy the main portion of Gelmandeh complex, which consists of hornblendite, garnet amphibolites, and gneiss. Geochemical investigations indicate that the ratio of Eu/Eu* separates samples into two categories: first category with ratio of Eu/Eu* > 1 and the second with ratio of Eu/Eu* °C.