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The Rock Dam Gold Prospect/A New Quartz Locality, Dickinson Co., Michigan

机译:密歇根州迪金森县,岩石坝金矿前景/新的石英位置

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The Rock Dam gold prospect is located in central Dickinson County, Michigan, approximately ten kilometers north of the village of Quinnesec (See map on page 5). The diggings (test pits and short adits) are developed in outcrops of the Early Proterozoic Sturgeon Quartzite Formation (Marquette Range Supergroup), the dominant exposed bedrock in this part of the county. Excavated near the turn of the 20th century, the prospects themselves are thoroughly unglamorous, yielding neither quartz crystals nor any noteworthy accessory minerals save muscovite and minor pyrite. Of these prospects, Bayley (1904) states that, "some of these quartz veins contain small quantities of free gold, as does also the quartzite in their vicinity." However, newspaper clippings from 1881 wax skeptical, saying that, ". . .quartz has been found and samples assayed which panned out at the rate of 1,000 dollars per ton, or big lies told. We are not quite certain which." (Cummings, 1991).
机译:岩坝金矿探矿场位于密歇根州的狄金森县中部,距昆尼塞克村以北约10公里(请参阅第5页的地图)。挖掘物(试验坑和短坑)是在该地区这一地区主要的裸露基岩-原始元古代St鱼石英岩层(Marquette Range Supergroup)的露头中发育的。在20世纪之交附近发掘时,前景本身就完全没有魅力,除了白云母和次要的黄铁矿,都没有产生石英晶体或任何值得注意的辅助矿物。在这些矿床中,Bayley(1904)指出:“这些石英脉中的一些含有少量的游离金,附近的石英岩也含有少量。”然而,1881年的报纸剪报对此持怀疑态度,他说:“发现了……石英,并分析了以每吨1,000美元的价格淘出的样本,或者说是大谎。我们还不确定哪一个。” (Cummings,1991)。

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