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产状与地质主要铜矿产地有比哈尔邦辛格伯哈姆和克赫特里铜带,另一些可采矿床分布在安得拉邦(阿格尼康拉)、梅拉鲁姆、卡纳塔克邦(迈索尔)和中央邦(玛兰克汗)。比哈尔的辛格伯哈姆铜带是长约140公里的辛格伯哈姆剪切破碎带的一部分。含矿岩系已发生剧烈形变,属前寒武纪铁矿系,含有黑云母、绿泥片岩、千枚岩、石英岩、角闪片岩;主要硫化矿物有黄铜矿、黄铁矿、磁黄铁矿、镍黄铁矿。该铜带的主要矿山有莫萨贝尼、色达、帕特哈哥拉、拉克哈和查普里。克赫特里铜带从辛格哈纳(昌昌努行政区)延伸至拉哈纳特加(锡卡尔行政区),长约80公里。
Producing and geology The major copper mines are the Sigharbollah and Khutrli copper belts in Bihar and other mineral deposits in Andhra Pradesh (Agnicon), Melaka, Natak (Mysore) and Madhya Pradesh (Khan Khan). The Sindhmbham copper belt in Bihar is part of the Sindhmbham shear fracture about 140 km in length. The ore-bearing rocks have undergone severe deformation and belong to the Precambrian iron ore system, which contains biotite, chlorite schist, phyllite, quartzite and hornblende. The main sulfide minerals include chalcopyrite, pyrite, Mine, nickel pyrite. The copper mine’s main mines are Mozambique, Seda, Patha Gora, Rakha and Chapuri. The copper belt of Khutrili extends from Singhhana (Changcharnu Administrative Region) to Lahanta Tengah (Chikarur Region) about 80 km in length.