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为配合地质找矿工作,1957年我们在清原矿区跳石背地区及矿区外围进行了4.8平方公里物探精查和120平方公里物探普查工作.在全部测区内进行了金属测量工作,获得了一定的地质效果.为进一步开展金属测量工作,提高普查找矿的效果和质量,现将此次工作成果及作法做如下介绍,供大家参考.一、区域地质简述矿区主要构造有浑河大断裂(约呈东西向),并有与其成锐角、近乎平行的“羽毛状”断裂(多在北侧).这组北东走向的断裂与浑河大断裂的形成有
In line with the geological prospecting work, we conducted the geophysical survey of 4.8 square kilometers and the geophysical survey of 120 square kilometers in the area of Caoshikou of Qingyuan Mining Area and the periphery of the mining area in 1957. We conducted metal surveys in all the surveyed areas and obtained certain Of the geological effects.To further carry out the work of metal measurement and improve the quality and effect of census prospecting, now the work achievements and practices are as follows, for your reference.Organization of regional geology The main structure of the mining areaHuhe large faults (Approximately east-west), with “feather-like” faults (more on the north side) that are at an acute angle and nearly parallel to each other.The north-easterly faults and the Hunhe big fault form