مرور Volume 9, Issue 1 بر اساس تاریخ انتشار
در حال نمایش موارد 1 - 5 از 5
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Petrogenesis of mantle peridotites from the South of Jazmourian, Makran accretionary prism, Iran
(Islamic Azad University, Mashhad Branch, 2017-04-01)Mantle peridotites exposed in south Jazmourian comprise of lherzolite and porphyroclastic Cpx-bearing harzburgite in the lower part with chromitite lenses in the upper parts. Petrography and microprobe studies shows evidence ...
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Delineation of enriched zones of Mo, Cu and Re by concentration-volume fractal model in Nowchun Mo-Cu porphyry deposit, SE Iran
(Islamic Azad University, Mashhad Branch, 2017-04-01)The purpose of this study is to identify the enriched zones of Cu, Mo and Re in Nowchun Mo-Cu porphyry deposit (SE Iran) based on subsurface data and using of concentration–volume (C–V) fractal model. The C-V model illustrates ...
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Pliocene volcanic activity of the Harrat Ash-Sham, South of Syria: geochemistry and petrogenesis
(Islamic Azad University, Mashhad Branch, 2017-04-01)The Cenozoic volcanic activity of the Harrat Ash Sham volcanic field in south of Syria is a part of the extensive magmatism that took place in the auxiliary extension faults along the Dead Sea Fault Zone from upper Eocene ...
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The Microbiostratigraphy and Depositional History of the Turonian–Santonian Surgah Formation at the Northern Flank of the Kuh-e Sepid Anticline, Lorestan Basin
(Islamic Azad University, Mashhad Branch, 2017-04-01)In this research, the microbiostratigraphy and depositional environmental implications related to the Surgah Formation at the northern flank of the Kuh-e Sepid anticline in the Lorestan Basin are discussed. A study of small ...
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Satellite thermal surveys to detecting hidden active faults and fault termination, Case study of Quchan fault, NE Iran
(Islamic Azad University, Mashhad Branch, 2017-04-01)The Quchan fault is located in Quchan - Shirvan area which is a part of Chenaran- Bojnourd plain in Kopeh-Dagh zone, NE Iran. The Quchan active fault with northwest – southeast trending is one of the most important strike-slip ...
