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首页> 外文期刊>Natural Resources Research >Mineral-Potential Mapping for MVT Deposits with Limited Data Sets Using Landsat Data and Geological Evidence in the Borden Basin, Northern Baffin Island, Nunavut, Canada
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Mineral-Potential Mapping for MVT Deposits with Limited Data Sets Using Landsat Data and Geological Evidence in the Borden Basin, Northern Baffin Island, Nunavut, Canada

机译:利用Landsat数据和地质证据在加拿大努纳武特北部巴芬岛Borden盆地进行的MVT矿床有限数据集的矿物潜力测绘

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摘要

Posterior probabilities of occurrence for Zn-Pb Mississippi Valley Type (MVT) mineralization were calculated based on evidence maps derived from regional geology, Landsat-TM, RADARSAT-1, a digital elevation model and aeromagnetic data sets in the Borden Basin of northern Baffin Island, Canada. The vector representation of geological contacts and fault traces were refined according to their characteristics identified in Landsat-TM, RADARSAT-1, DEM, slope, aspect, and shaded relief data layers. Within the study area, there is an association between the occurrence of MVT mineralization and proximity to the contact of platformal carbonates and shale units of the adjacent geological formation. A spatial association also tends to exist between mineralization and proximity to E-W and NW-SE trending faults. The relationships of known MVT occurrences with the geological features were investigated by spatial statistical techniques to generate evidence maps. Supervised classification and filtering were applied to Landsat-TM data to divide the Society Cliffs Formation into major stratigraphic subunits. Because iron oxides have been observed at some of the MVT occurrences within the Borden Basin, Landsat-TM data band ratio (3/1) was calculated to highlight the potential presence of iron-oxides as another evidence map. Processed Landsat-TM data and other derived geological evidence maps provided useful indicators for identifying areas of potential MVT mineralization.
机译:根据北巴芬岛北博登盆地的区域地质,Landsat-TM,RADARSAT-1,数字高程模型和航空磁数据集得出的证据图,计算了锌-铅密西西比河谷类型(MVT)矿化的后发生概率,加拿大。根据在Landsat-TM,RADARSAT-1,DEM,坡度,坡向和阴影起伏数据层中确定的特征,完善了地质接触和断层痕迹的矢量表示。在研究区域内,MVT矿化的发生与邻近相邻地层的平台碳酸盐岩和页岩单元的接触程度之间存在关联。矿化与接近E-W和NW-SE趋势断裂之间也存在空间联系。通过空间统计技术研究了已知MVT发生与地质特征的关系,以生成证据图。在Landsat-TM数据上进行监督分类和过滤,以将学会悬崖地层划分为主要地层亚单元。因为在Borden盆地内的某些MVT发生处已经观察到氧化铁,所以计算Landsat-TM数据带比率(3/1)可以突出显示氧化铁的潜在存在,作为另一个证据图。经过处理的Landsat-TM数据和其他衍生的地质证据图为确定潜在MVT矿化区域提供了有用的指标。

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