USE OF DIGITAL MODELS OF GEOLOGICAL STRUCTURE TO IDENTIFY PALEOVOLCANIC STRUCTURES CONTROLLING PORPHYRY ORE OBJECTS

S. V. Efremov, N. Goryachev, A. Budyak, S. Y. Skuzovatov, A. V. Blinov
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Abstract

The article is devoted to the implementation of the methodology for paleovolcanic structure analyzing using 3D visualization of the model of the geological territory structure based on the relief digital model. The approach used made it possible to identify two paleovolcanic apparatuses and their structural elements: cone fragments, explosive domes, porphyritic stocks, ring fault zones with localization of dike belts in them. This, within the framework of the evolution model of porphyry ore systems, made it possible to identify promising areas for prospecting on ore objects of a given type. The procedure was checked on the basis of geochemical survey results. The regular control by the selected structural elements of geochemical fields was shown. The analysis of the spatial position of the selected structural blocks with a certain geochemical characteristic rather well into the evolution model of the porphyry ore systems. In all cases the control of geochemical halos by porphyry stocks is noted, the material rock complexes that are fragments of the zonal stone hat of the porphyry ore object, are quite clearly distinguished. Within the area of work, three ore-magmatic systems can be identified at a low level of erosion shear, potentially accompanied by porphyry-type ore mineralization.
利用地质结构数字模型确定控制斑岩矿体的古火山结构
文章主要介绍了利用基于浮雕数字模型的三维可视化地质区域结构模型分析古火山结构的方法。所使用的方法可以确定两个古火山装置及其结构元素:锥体碎片、爆炸穹隆、斑岩储量、环状断层带以及其中的堤坝带定位。在斑岩矿石系统演化模型的框架内,这样就有可能确定对特定类型矿石进行勘探的有利区域。根据地球化学勘测结果对该程序进行了检验。结果表明,选定的结构元素对地球化学领域有规律的控制。对具有特定地球化学特征的选定构造块空间位置的分析,很好地反映了斑岩矿系统的演化模型。在所有情况下,地质化学晕都受到斑岩储量的控制,斑岩矿石对象的带状石帽碎片的物质岩石复合体也被清楚地区分出来。在工作区域内,可以在侵蚀剪切程度较低的地方发现三个矿石-岩浆系统,可能伴有斑岩型矿化。
本文章由计算机程序翻译,如有差异,请以英文原文为准。
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