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作 者:李洪涛 LI Hong-tao(Second regional geological survey brigade of Xinjiaag Bureau of Geology and mineral resources,Changji 831100,China)
机构地区:[1]新疆地矿局第二区域地质调查大队,新疆昌吉831100
出 处:《世界有色金属》2017年第6期171-171,173,共2页World Nonferrous Metals
摘 要:西天山地区矿产资源丰富,在已发现的各类矿中,尤以铁矿最为重要,博罗科努山系是该类铁矿的主要分布区域,由于铁矿资源非常丰富,不仅是西天山地区,也是整个新疆地区非常重要的铁矿成矿区带。本文研究的查岗诺尔铁矿,其地理位置就分布在西天山地区,属于该区的中部区域,博罗科努山系的中间主脊线就是该矿的分布地区,是中天山北缘区域内的活动陆缘带对该矿床而言前人再此开展过很多地质研究工作,文中笔者结合前人的研究成果,总结了查岗诺尔铁矿的矿床成因和成矿模式,提出了找矿标志,预测了同类矿床的有利地段。The mineral resources in West Tianshan Mountains is rich, have been found in all kinds of ores, especially iron ore is the most important, Boluo is the main distribution area of the wild mountain iron ore, the iron ore resources are very rich, not only is the Western Tianshan area, but also the entire area of Xinjiang iron ore district is very important with. This paper studies the Chagannur iron ore, its geographical location is distributed in the Western Tianshan area, the central region belongs to the area of Boluo mountains, Kono main ridge line is the middle of the mine area, is in the Northern Tianshan region of active continental margin zone of the deposit for the previous development of many geological research the results of previous research work, the author in this paper, summed up the ore genesis and metallogenic model of Chagannur iron ore, proposed for prospecting prediction of favorable area for similar deposits.
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