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Iron Hill carbonatite

机译:铁山碳酸盐岩

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The Iron Hill carbonatite complex is a 31km~2 alkalic intrusion at Powderhorn, approximately 35km south-south/west of Gunnison, Colorado, USA. Originally explored for its iron deposits, Iron Hill is now coveted for its vast reserves of titanium, estimated to be half of the USA's usable total. Teck Comico Ltd, Vancouver based precious metals and minerals miners, has had 100 percent ownership of the complex since 1994. The primary rock types Iron Hill are pyroxenite, uncompahgrite, ijolite, nepheline syenite and carbonatite. These bodies of rock intruded into the region approx 570 Ma into Early Proterozoic granite and syenite and older Proterozoic metamorphic rocks.
机译:Iron Hill碳酸盐岩复合体是在美国科罗拉多州甘尼森市以南/西南约35公里处Powderhorn的31km〜2碱性侵入岩。最初因铁矿开采而被探寻,如今因其庞大的钛储量而备受追捧,据估计,铁储量占美国可用总量的一半。自1994年以来,位于温哥华的Teck Comico Ltd公司就一直拥有该金属矿山的100%所有权。铁山的主要岩石类型为辉石岩,辉绿岩,白云母,霞石正长岩和碳酸盐岩。这些岩石体侵入了大约570 Ma的区域,进入了早期元古代花岗岩和正长岩以及较古老的元古代变质岩。

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