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PREDICTION METHOD HIDDEN MINERALIZATION ASSOCIATED WITH granitoids

机译:花岗岩类隐伏矿化的预测方法

摘要

Method prediction latent mineralization associated with granites, characterized in that for prospective mineralized portions is performed based on the physical rock properties, data composing a model sectional view and materials of small-scale gravirazvedochnyh and magnitorazvedochnyh filming construction "zero" depth model in the form of deep cuts in are all identified bodies assigned corresponding range of variation of density and magnetic characteristics, and then through a series of solutions of inverse problems performed interactively selection depth model in which change as a form of individual bodies model and their physical properties (density and magnetization) until practically complete coincidence of calculated gravitational and magnetic fields with observations obtained inhomogeneous distribution of rock density and magnetization interpreted using reference genetic model ore-magmatic systems, with the construction of geological and geophysical sections in which at sharp change or shift of contour field density and nama ness isolated major faults and low-density nonmagnetic field rocks as residual foci cotectic granites (sources fluids ore material and energy), and extending from them apophyses contoured as projected ore deposition zone.
机译:预测与花岗岩有关的潜在矿化作用的方法,其特征在于,根据岩石的物理性质,构成模型剖面图的数据以及小规模gravirazvedochnyh和magnitorazvedochnyh成膜构造“零”深度模型的材料来进行潜在矿化部分的预测所有被识别的物体都进行了深切,并为其分配了相应的密度和磁特性变化范围,然后通过一系列反问题的解决方案以交互方式进行选择深度模型,其中以个体物体模型及其物理特性(密度和密度)的形式变化磁化强度),直到计算出的重力和磁场与观测值几乎完全吻合为止,获得的岩石密度和磁化强度的不均匀分布是使用参考遗传模型矿石-岩浆系统解释的,其中地质和地球物理部分的构造在等高线场密度和纳米度的变化或偏移将主要断层和低密度非磁场岩石隔离为残留的焦点共晶花岗岩(为流体矿石材料和能量提供来源),并从中延展出轮廓如投影矿石沉积带的复生岩。

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