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阿巴坎铁矿床与阿巴津钠长石的侵入有关,属接触交代型矿床,其上部的磁铁矿矿化带有两个代表性矿体,主矿体和3号矿体,前者集中全部储量的90％。矿体为北东走向,长1200米(在地表),大体呈垂直延深,矿体地表露头顶端的标高为+822米,在标高+120米尖灭。水平厚度为0～190米。围岩是以凝灰岩、砂质粘土页岩和石灰岩为代表的沉积凝灰岩。最初苏联国家矿产委员会批准的储量在矿床上部为8650万吨,而1982年1月1日减为4060万吨。矿床的特点是矿石坚硬,围岩稳固,受
The Abakan iron ore deposit is related to the invasion of abamectin albite, belonging to the contact metasedimentary deposit. The upper part of the magnetite mineralization has two representative ore bodies, the main orebody and the No.3 orebody, the former Concentrate 90% of all reserves. The ore body is northeastward and 1200 meters long (on the earth’s surface), with a generally vertical extension. The elevation at the top of the outcrop of the ore body is +822 meters and pinch out at the elevation of +120 meters. The horizontal thickness of 0 to 190 meters. Surrounding rock is tuff, sandy clay shale and limestone as the representative of the sedimentary tuff. The reserves initially approved by the Soviet National Mineral Council were 86.5 million tonnes in the upper part of the deposit, down from 40.6 million tonnes on January 1, 1982. The deposit is characterized by hard ore, rock solid, subject to