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作 者:刘国印[1] 燕长海[1] 赵建敏[1] 王纪中[2] 李中明[1]
机构地区:[1]中国地质大学,北京100083 [2]河南省地质调查院,河南郑州450007
出 处:《地质通报》2008年第5期641-648,共8页Geological Bulletin of China
基 金:中国地质调查局国土资源调查项目《河南陕县-新安-济源地区铝土矿调查评价》(编号:1212010532403);河南省两权价款项目《河南省重要成矿区带1:5万区域矿产调查》资助。
摘 要:通过方法试验,在豫西地区已知铝土矿区的外围开展了1:5万高精度重力测量,发现绝大多数矿床点位于较平缓的重力梯度带上,基底相对稳定的地段可作为铝土矿的找矿靶区;采用CSAMT(可控源音频大地电磁)法测深剖面,卡尼亚电阻率-频率曲线拐点可直接反映出新生界覆盖层和奥陶系灰岩层的埋藏深度,进而推断石炭系本溪组(铝土矿)的埋深。经10余个钻孔验证,见矿率达80%以上。试验结果证明,在地质研究的基础上,微重力法加上CSAMT法测深是寻找隐伏铝土矿的有效的方法组合。The authors carried out 1:50000 high-precision microgravity survey through methodological experiments at the peripheries of the known bauxite mining area in western Henan and found that most ore deposits are located in gentle gravity gradient zones and that areas with a comparatively stable basement are bauxite exploration targets. The burial depths of the Cenozoic cover (aluminiferous rocks) and Ordovician limestone (dolostone) bed can be directly reflected by the controllable source audio frequency magnetotelluric (CSAMT) sounding section and Kania resistivity-frequency curve inflexion and then further the burial depth of the carboniferous Benxi Formation (bauxite) may be deduced. Checks and verification of more than ten boreholes show that the ore encountering rate reaches more than 80%. The results of tests prove that the combined microgravity survey and CSAMT sounding carried out based on the geological study are an effective technique combination for looking for hidden bauxite deposits in western Henan.
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