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Abstract
Aspects in Mining & Mineral Science
The Manto-Type Copper Mineralization in the Eocene Volcano-Sedimentary Sequences, Western Alborz-Azarbayjan Belt, NW Iran
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Open or CloseGhasem Nabatian*
Department of Geology, Faculty of Sciences, Iran
*Corresponding author: Ghasem Nabatian, Department of Geology, Faculty of Sciences, University of Zanjan, Zanjan, Iran
Submission: April 05, 2021; Published: June 02, 2021
ISSN : 2578-0255Volume6 Issue5
Abstract
Iran is located in the middle part of the Alpine-Himalayan orogenic belt and resulted from the evolution of the at least three Tethyan oceans (Proto, Paleo and Neo-Tethys). The evolution of Tethyan oceans caused to formation of different types of mineralization in Iran during Precambrian- Cambrian to recent time. The manto-type copper deposits is one of the most important deposits in Iran which occurred within the Urumieh-Dokhtar Magmatic Arc (UDMA), Lut block, Sanandaj-Sirjan Magmatic-Metamorphic Zone (SaSZ), Sabzevar subzone and mainly Alborz Magmatic Belt (AMB).
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