摘要
<正>南岭地区历经多期次构造岩浆活动,多金属成矿条件优越~([1]),是世界上研究燕山期花岗岩成矿理论最典型区域之一,圈定隐伏花岗岩体的分布范围对成矿预测具有重要意义。根据物性资料统计显示,区内花岗岩呈低密度特性,但是由于区域背景场的叠加,不同深源层异常的复合,使得岩体重力异常弱缓、混叠,导致传统位场构造识别方法(垂向二次导数,总梯度模,解析信号振幅谱,Tilt梯度)效
引文
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