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前言赫姆洛金矿床发现于1982年,它位于苏必利尔湖东北岸附近,马拉松东15公里与横贯加拿大的17号公路邻接,其地理座标北纬48°40″,西经86°00″。主矿带走向为115°,倾向在50°—70°之间。矿床由几个矿化带组成,延伸长为1300米,垂直深度1300米,厚度变化范围3—45米。部分矿床出露地表,看来是单一大矿床,至少有7千万公吨金矿石,平均品位为7.6g/t,直到经过地下开采检验后,才能确定各个矿体的连续性,矿床包括三部分:泰克-科罗纳,金巨人和帕格-威廉斯。
Foreword The Hermione gold deposit was discovered in 1982 and is located near the northeastern shore of Lake Superior, 15 kilometers east of Marathon adjoins Route 17 across Canada and has a geographical coordinates of 48 ° 40 "north latitude and 86 ° west longitude. The main ore strike is 115 ° with a dip of 50 ° -70 °. The deposit consists of several mineralized zones with an extension of 1,300 meters and a vertical depth of 1,300 meters with varying thickness ranging from 3 to 45 meters. Some of the deposits are exposed to the surface and appear to be a single large deposit with at least 70 million tonnes of gold ore at an average grade of 7.6 g / t. The continuity of individual ore bodies can not be determined until underground mining has been conducted. The deposit consists of three parts : Tektronix - Corona, Golden Giant and Pug-Williams.