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萨尔切什迈钢矿床在全世界可居第三或第四位,至少含有4.27亿吨铜矿石,平均品位为1.13％Cu、0.03％Mo。进一步的钻探作业有可能使矿石储量增至8亿吨,使金属铜含量从530万吨增至1000万吨。就金属铜量来说,萨尔切什迈低于其它三个斑岩铜矿床;智利的埃尔台尼特矿山(3150万吨);丘基卡马塔(3000)万吨以上),美国肯尼考特公司的宾厄姆坎扬(粗估为1000万吨)。该矿床的钼台量随深度不断增加。萨尔切什迈铜矿位于扎格罗斯山脉中部,是一个北北西—南南东走向的矿带,由早第三纪火山一沉积岩组成,该带从土耳其延伸至伊朗南部的俾路支。该带的西南侧是一个大型俯冲带,许多人都认为,这标志着西部阿拉伯板块与东部喜马拉雅板块的边界。在俯冲带的东部见有与潜没带有关的大陆地台型火山沉积物,而在西南部则有
The Salcheshmai steel deposit is the third or fourth largest in the world with at least 427 million tonnes of copper ore with an average grade of 1.13% Cu and 0.03% Mo. Further drilling operations have the potential to increase ore reserves to 800 million tons and copper metal content from 5.3 million tons to 10 million tons. In terms of metal copper, Salcezimé is lower than the other three porphyry copper deposits; El Niño mines in Chile (31.5 million tons); Chuqui Kamata (3000 million tons) Bingham Canyang, Kenny Court of the United States (estimated at 10 million tonnes). The molybdenum level of this deposit is increasing with depth. Located in the center of the Zagros Mountains, the Salchezmei copper mine is a north-west-south-south-east ore belt composed of Early Tertiary Volcano-Sedimentary rocks extending from Turkey to Balochistan in southern Iran. On the southwestern side of the belt is a large subduction zone, which many see as a sign of the border between the western Arabian plate and the eastern Himalayan plate. In the eastern part of the subduction zone, there are continental platform volcanic sediments related to the subduction zone, while in the southwest there are