Heterodera sp. Urumieh-SS-2002
National Institutes of Health
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The Chah-Shur clay deposit is located in 150 km southeast of Isfahan. Eocene igneous rocks and Quaternary deposits cover the area…
The Sanandaj‐Sirjan zone of Iran is a northwest trending orogenic belt immediately north of the Zagros suture, which represents…
Iranian Cenozoic magmatic belt, known as Urumieh-Dokhtar, is recognized as an important polymetallic mineralization which hosts…
This study presents the applicability of recently launched Landsat-8 data for hydrothermal alteration and lithological mapping…
The Lalezar granitoids crop out within volcanic successions of the Urumieh-Dokhtar Magmatic Assemblage (UDMA). These granitoids…
Urumieh-Dokhtar Magmatic Arc (UDMA) is
known as a belt with copper and some other metal deposits. The study
area is a part of…
Kahang Cu Porphyry deposit is situated in the central part of a major Iranian magmatic belt, Urumieh-Dokhtar, in central Iran…
Pleistocene basaltic lava flows, consisting of trachybasalt and basaltic trachyandesite, cover an area north-northwest of Shahre…
A multidisciplinary study including field geology, microstructure analysis, 40Ar/39Ar dating, and fluid inclusion…