Pressure, temperature and oxygen fugacity conditions of Ganj dioritic-quartz dioritic intrusives, west of Makran, and its tectonomagmatic implication
Pressure, temperature and oxygen fugacity conditions of Ganj dioritic-quartz dioritic intrusives, west of Makran, and its tectonomagmatic implication

Alireza Shaker Ardakani; Mohsen Arvin; Sara Dargahi

Volume 7, Issue 25 , April 2016, , Pages 51-64

https://doi.org/10.22108/ijp.2016.20832

Abstract
  The Ghaleh-Ganj dioritic- quartz dioritic massifs, with the age of Paleocene-Eocene, located on the west side of the Makran accretionary prism and Jazmurian depression and the east ...  Read More
Morphological, structural, textural and mineralogical evidences of pillow lavas from Ganj complex, Southeastern Kerman
Morphological, structural, textural and mineralogical evidences of pillow lavas from Ganj complex, Southeastern Kerman

Alireza Shaker Ardakani; Mohsen Arvin; Roland Oberhänsli

Volume 1, Issue 3 , December 2010, , Pages 47-64

Abstract
  The Makran accretionary prism in southeastern Iran contains extensive Mesozoic melange zones and large intact ophiolites, representing remnants of the Neotethys oceanic crust that was ...  Read More