نتایج جستجو برای: sirjan metamorphic belt
تعداد نتایج: 22078 فیلتر نتایج به سال:
تکامل گرمابیها بر اساس بررسیهای کانیشناسی و میانبارهای شاری در کانسنگهای آهن قطروئیه، استان فارس
The Qatruyeh iron occurrences are located in the eastern edge of the Sanandaj-Sirjan metamorphic zone, southwestern Iran (at 50 Km northeastern of Neyriz), and are hosted by a Late Proterozoic to Early Paleozoic sequence which is dominated by metamorphosed carbonate rocks. The Iron ores occur as layered, massive and disseminated magnetite and in lesser amount as hematite-bearing veins and veinl...
Mollataleb area is located in the north of Aligudarz city, in the Sanandaj-Sirjan metamorphic zone. The regional metamorphic rocks with Upper Triassic-Jurassic age and various granitoid units are the most important geological event that occurred in the area. The development of granitoid masses in Aligudarz area aged Middle Jurassic that intruded into schists. Microprobe analyses of tourmalines ...
Ophiolitic rocks in the southeastern part of the Zagros Orogenic Belt can be separated from southwest to northeast, into two groups: the Neyriz ophiolites and the Naien–Shahrebabak–Baft ophiolites. The southeast sector of Sanandaj-Sirjan wasdelimited by the two nearly synchronous ophiolitic belts in its southwestern and northeastern margins. In this study, new ophiolitic formation models were u...
Late Neoproterozoic-Early Cambrian schists have been occurred in southwest of Zanjan city from the Soltanieh belt. The Soltanieh belt in northwest of Iran is uplifted basement of Precambrian-Paleozoic in main central Iran zone and includes outcrops of Precambrian, Paleozoic and Mesozoic Formations. Late Neoproterozoic-Early Cambrian schists, the oldest stratigraphy unit in the region, consist o...
The study area is a part of so-called Sanandaj-Sirjan zone or Zagros imbricate zone of the Zagros Orogen, Iran. The Hamedan region comprises a metamorphic sequence of low- to high-grade regional and contact metamorphic rocks intruded by mafic, intermediate and felsic plutonic bodies. The sequence comprises pelitic, psammitic, mafic, calc-pelitic and calc-silicate rocks. Pelitic rocks are the m...
Structural and metamorphic analyses of the Porto–Viseu Metamorphic Belt (PVMB), an anatectic complex located in Central-Iberian Zone (CIZ), Iberian Variscan Massif, constrain kinematic features polyphase deformation, as well boundary conditions associated with exhumation emplacement belt onto CIZ’s lower-grade metasediments. A sharp contrast is evident between lowest grade rocks complex—garnet-...
Trends in Textile Engineering & Fashion Technology A Mini-Review of Using Additive Manufacturing the Industry? Behnam Akhoundi* and Ahmad Mashayekhi Department Mechanical Engineering, Sirjan University Technology, Sirjan, Kerman Province, Iran *Corresponding author:Behnam Akhoundi, Submission: December 14, 2022; Published: January 13, 2023 DOI: 10.31031/TTEFT.2023.07.000674 ISSN 2578-0271 Volum...
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