Volume 32 (2022)
Volume 31 (2021)
Volume 30 (2020)
Volume 29 (2020)
Volume 28 (2019)
Volume 27 (2018)
Volume 26 (2017)
Volume 25 (2016)
Volume 24 (2015)
Volume 23 (2014)
Volume 22 (2013)
Volume 21 (2012)
Volume 20 (2011)
Volume 19 (2010)
Volume 18 (2009)
Volume 17 (2008)
Volume 16 (2007)
Investigation of geomorphological changes and sediment characteristics of Napag mud volcano, Makran, Iran

K. Nezhadafzali; R. Lak; M. Ghoreshi

Volume 26, Issue 104 , September 2017, , Pages 261-266


  Mud volcano is a natural and spectacular phenomenon that usually appear in form of a dome but some are found as a basin. Mud volcanoes comprise a mixture of water, gas and mud. They are found in most parts of the world, particularly in the Alps and Himalayas belts.  In Iran, most of the mud volcanoes ...  Read More

Love wave tomography of the Makran subduction zone from ambient seismic noise

M Abdetedal; Z.H Shomali; M.R Gheitanchi

Volume 26, Issue 102 , March 2017, , Pages 147-152


  The Makran zone in southeastern Iran and southern Pakistan is the result of subduction of oceanic crust of the Arabian Plate under the Eurasian Plate. From seismic behavior point of view, there is a distinct segmentation between the western and eastern parts of the subduction zone. The western part of ...  Read More

Sedimentology and Geochemistry of Siliciclastic Sediments (Tertiary-Quaternary) in the Eastern Coasts of Chabahar, SE Sistan and Baluchistan

M Afarin; M Boomeri; A Mahboubi; M Gorgij; M.A Hamzeh

Volume 24, Issue 96 , September 2015, , Pages 85-97


  In this study, geochemical and sedimentological assessment was carried out on mudstone and sandstone deposits of Eastern coasts of Chabahar. Fifty samples were taken from five  sectione of Tiss, Ramin, Lipar, Gorankesh and Garindar estuary and subjected to grain size analysis and chemical analysis ...  Read More

Geochemistry and Petrogenesis of Ghaleh-Ganj Dioritic- Quartzdioritic Plutonism, Southeast of Kerman

A.R Shaker Ardakani; S Dargahi; H Amirpour

Volume 24, Issue 94 , March 2015, , Pages 147-156


  The Ghaleh-Ganj dioritic- quartzdioritic massifs, Post early Eocene in age, located on the west side of the Makran Accretionary Prism and the Jazmurian Depression and the east side of the Jiroft fault, are part of the intrusives in the Ganj Complex, which itself is a part of the Jazmurian Ophiolitic ...  Read More

Petrography, Mineral Chemistry and Petrogenesis of the Ganj Complex Felsic Plutonic Rocks, South East of Iran: Constraints on its Tectonic Environment

A Shaker Ardakani; M Arvin; B Oberhänsli

Volume 23, Issue 92 , September 2014, , Pages 143-154


  The Lower Paleocene felsic plutonic rocks in the N- NE of Ghaleh-Ganj, are located on the western side of the Makran accretionary prism and the Jazmurian Depression and the east side of the Jiroft fault. They are parts of the intrusives in the Ganj complex, which itself is a part of the Jazmurian ophiolitic ...  Read More

Petrology and Geochemistry of Peridotites fromFannuj-Maskutan Ophiolitic Complex, Makran Zone, SE Iran

M. E. Moslempour; M. Khalatbari-Jafari; T. Morishita; M. Ghaderi

Volume 22, Issue 87 , December 2013, , Pages 181-196


  Mantle sequences exposed in west of Fannuj-­Maskutan area comprise of lherzolite and porphyroclastic cpx-bearing harzburgite in the lower part and recrystallized fine-grained lherzolite with chromitite lenses in the upper parts of the sequence. Petrography studies and microprobe data show evidence ...  Read More