Fluorite vein mineralization occurs mainly in slates and phyllites of Lower Jurassic
Shemshak Formation and scarcely in Triassic limestones in Bozijan, which is situated at the …

Barite mineralization occurs at Chenarvardeh deposit as layers and lenses in Upper Eocene
volcanic and pyroclastic rocks. The host rocks are intensely saussuritized in most places …

The Qahr-Abad fluorite deposit in western Iran is characterized by fluorites that mainly occur
as veins, veinlets, and open-space fillings in dolomitic host rocks of the Triassic Elika …

Subduction of Neo-Tethyan oceanic crust and the subsequent continental collision has
created important geological features along the Alpine-Himalayan orogenic belt, including …

Abstract The Nohkouhi copper deposit (1.5 Mt@ 1% Cu) is the first reported VMS deposit
among several SEDEX deposits in Posht-e-Badam block, Central Iran. The deposit is …

Fluorite vein mineralization has mainly occurred in carbonate rocks of the Triassic Elika
Formation in the Qahr-Abad district, situated southeast of the city of Saqqez in western Iran …

Abstract The Sarvian Fe skarn deposit is located in the Urumieh–Dokhtar magmatic arc,
western Iran. The Sarvian quartz diorite intruded the surrounding Permian to Tertiary limy …

Introduction The Aqkand Cu occurrence, 48 km north of Zanjan, is located in the Tarom
subzone of the Western Alborz-Azerbaijan structural zone. Apart from small scale geological …

The Cenozoic magmatism is mainly concentrated in the Alborz magmatic arc, Urumieh-
Dokhtar magmatic arc, Central and Eastern Iran. The Western Alborz magmatic arc known …

Mashayekh area is located in Charmahal and Bakhtiari province and is structurally located
in the high Zagros belt. This region is characterized by two mining districts, namely, the …