Volume 13 (2022)
Volume 12 (2021)
Volume 11 (2020)
Volume 10 (2019)
Volume 9 (2018)
Volume 8 (2017)
Volume 7 (2016)
Volume 6 (2015)
Volume 5 (2014)
Volume 4 (2013)
Volume 3 (2012)
Volume 2 (2011)
Volume 1 (2010)
Author = Torabi, Ghodrat
Number of Articles: 16
A study of the Eocene S-type granites of Chapedony metamorphic core complex (northeast of Yazd province, Central Iran)
Volume 7, Issue 25 , April 2016, , Pages 33-50
Abstract
The Eocene Chapedony metamorphic core complex, is located in western part of the Posht-e-Badam block. This complex is consisting of migmatite, gneiss, amphibolite, marble, micaschist ... Read MorePetrography and mineral chemistry of volcanic rocks in Kuh-e-Siah (North of Gavkhuni lagoon, SE of Isfahan)
Volume 4, Issue 15 , March 2014, , Pages 17-38
Abstract
Kuh-e-Siah is located in the north of Gavkhuni lagoon and east of the Varzaneh (SE of Isfahan) and is a part of Urumieh-Dokhtar magmatic arc (UDMA). The volcanic rocks of this area ... Read MorePetrology of Toveireh alkaline basalt an evidence of within-plate Oligocene volcanism in the northwest of Central-East Iranian Microcontinent, southwest of Jandaq
Volume 4, Issue 16 , February 2014, , Pages 21-38
Abstract
In the northwest of the Central-East Iranian Microcontinent (CEIM), southwest of Jandaq, the Toveireh Oligocene alkaline basalt with NW-SE to W-E trend is outcropped. This alkaline ... Read MorePetrography and mineral chemistry of the Eocene volcanic rocks in the Posht-e-Badam block
Volume 4, Issue 14 , July 2013, , Pages 31-48
Abstract
The Eocene volcanic rocks of the Posht-e-Badam block represent very good exposures in Saghand (Khoshoumi Mountain), Alahabad and Chapedony areas (Yazd province). These rocks were developed ... Read MorePetrography and mineral chemistry of Eocene dykes from Kuh-e-Kam Khashak (North of Khur, Isfahan province)
Volume 4, Issue 13 , April 2013, , Pages 19-32
Abstract
Ku-e-Kam Khashak is located in the NE of Isfahan (North of Khur). Basic dykes trending NE-SW and intermediate dykes with NW-SE trend cross cut the Upper Cretaceous sandstone, limestone ... Read MoreStudy of mantle peridotites of Surk ophiolitic melange (Yazd province, Iran)
Volume 3, Issue 12 , March 2013, , Pages 51-68
Abstract
The Surk ophiolitic melange, as a narrow belt, is located in western part of Yazd province, between the southwest of Central Iran and Urumieh-Dokhtar magmatic arc, along Naein-Dehshir-Baft ... Read MoreMetamorphism of mantle peridotites in Jandaq ophiolite (Central Iran)
Volume 3, Issue 11 , December 2012, , Pages 1-18
Abstract
Jandaq ophiolite is one of the old ophiolites in Iran belonging to Proterozoic and Paleozoic, and subjected to different phases of metamorphism. The studied ophiolite is covered by ... Read MoreMineralogical study of metabasites in Me'raji and Chah Palang Mountains (South of Chupanan, NE Isfahan province)
Volume 3, Issue 10 , December 2012, , Pages 27-44
Abstract
The metabasites of Me'raji and Chah Palang Mountains located south of Chupanan (Central Iran) and covered by the Paleozoic metamorphic complexes. These metabasites are composed of closely ... Read MorePetrography and mineral chemistry of Eocene volcanic in the southwest of Jandaq (northeast of Isfahan)
Volume 3, Issue 10 , December 2012, , Pages 95-107
Abstract
In the south west of Jandaq area, the Eocene volcanic rocks crop out, near the Doruneh Fault in a large area. These rocks are composed predominantly of basalt, quartz andesite, andesite, ... Read MorePetrology of Lower Cretaceous pillow lavas and diabase dykes from North of Hajiabad (SW of Bayazeh, Isfahan province, Iran)
Volume 2, Issue 8 , January 2012, , Pages 39-54
Abstract
The Lower Cretaceous pillow lavas and diabasic dykes are cropped out in several points in the North of Hajiabad belonging to Central Iran. The best exposure of these rocks is seen in ... Read MorePetrology of Mesr granitoid complex (NE of Isfahan Province)
Volume 2, Issue 6 , November 2011, , Pages 1-16
Abstract
The Mesr granitoid complex situated in the NE of Isfahan Province and from structural viewpoint belongs to Central Iran. In this area, three granitoid phases and one pegmatite phase ... Read MoreCauses of different composition of chromitites in Naein and Ashin ophiolites, and its absence in Anark and Jandaq ophiolites (Isfahan province)
Volume 2, Issue 7 , June 2011, , Pages 1-20
Abstract
There are two types of ophiolites in the west of Central Iran: Mesozoic ophiolites (Naein and Ashin), and Paleozoic or Precambrian ophiolites (Anarak and Jandaq). Field studies show ... Read MoreMineral chemistry of mantle peridotites from Loghar ophiolite (Southweast of Kabul - Afghanistan)
Volume 2, Issue 5 , June 2011, , Pages 19-48
Abstract
The Loghar ophiolite is located in ophiolitic belt of Kabul block (southeast of Afghanistan) and it is a part of Neotethyan ophiolites in Alpine - Himalayan orogenic system with Eocene ... Read MorePetrology of Devonian basalts from Pol-e-Khavand area (SE of Anarak, NE of Isfahan)
Volume 1, Issue 3 , December 2010, , Pages 29-46
Abstract
Volcanic rocks with composition of basalt and possibly Lower Paleozoic (Devonian) age are present in the Kuh-e-Abdulhosein (Pol-e-Khavand, Anarak area). These rocks with 120 m thickness ... Read MorePetrography and mineral chemistry of basaltic dykes in the west of Borooni (SW of Ardestan, Iran): evidences of magma mixing
Volume 1, Issue 2 , September 2010, , Pages 17-30
Abstract
In Borooni area (SW of Ardestan), which is a part of Uromiyeh â Dokhtar magmatic belt, the Miocene basaltic columnar-jointed dikes cross cut the Eocene volcanic rocks. These ... Read MoreGeochemistry and Petrogenesis of volcanic rocks from the Arousan-e- Kaboudan (NE of Anarak)
Volume 1, Issue 1 , June 2010, , Pages 103-120