THEORETICAL-METHODOLOGICAL AND CRITERION-CONCEPTUAL BASIS OF FORECASTING-METALLOGENIC RESEARCH

M. Pavlun
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Abstract

Theoretical-methodological and criterion-conceptual basis of forecasting-metallogenic researches, and also the maintenance and methods of drawing up of metallogenic and forecasting maps as the most important practical reflection of laws of space-time distribution of solid minerals deposits have been analysed. Deposits are formed due to certain combinations of geotectonic, geochemical, petrological and actually ore-forming processes. Knowledge of informative interpenetration and logical interaction of these processes determines the rationality, reliability and success of predictive research of potentially ore-bearing rock complexes. Metallogenic features, and hence the signs (criteria) of the manifestation of mineralization are always different at different stages of the geological history of the Earth's crust. Therefore, forecasting-metallogenic works should be performed taking into account only real, objectively available geological-geochemical and geophysical parameters of mineralization, which can be traced, documented, mapped and fully or as much as possible objectified in the process of compiling metallogenic and forecast maps. The metallogenic map shows the patterns of formation and localization of useful minerals, metallogenic zoning of the country or individual regions, the classification of metallogenic objects. In the case of such maps, two approaches are used: paragenetic (localization of deposits is determined on the basis of generalization of information about the confinement of deposits to certain geological formations and tectonic structures) and genetic (applied to sedimentary minerals that are part of the stratigraphic section and reflect sedimentation processes). Today, forecast maps are preferred because, unlike metallogenic ones, they reflect conclusions about possible, but not yet discovered ore-bearing areas and deposits, their long-term assessment, often with a description of their species and sequence. In fact, the forecast map is not one map, but a set of maps with a corresponding explanatory note.
预测成矿研究的理论方法和标准概念基础
分析了成矿预测研究的理论方法和标准概念基础,以及作为固体矿床时空分布规律最重要的实际反映的成矿预测图的维护和编制方法。矿床是由于大地构造、地球化学、岩石学和实际成矿作用的某种组合而形成的。对这些过程的信息互贯和逻辑相互作用的认识,决定了潜在含矿岩杂岩预测研究的合理性、可靠性和成功性。在地壳地质历史的不同阶段,成矿特征和矿化表现的标志(标准)总是不同的。因此,成矿预测工作应只考虑真实、客观可得的成矿地质地球化学和地球物理参数,在编制成矿预测图的过程中,这些参数可以被追踪、记录、作图,并充分或尽可能地客观化。成矿图显示有用矿物的形成模式和定位,国家或个别地区的成矿分区,成矿对象的分类。在这种地图的情况下,使用了两种方法:共生法(根据关于矿床局限于某些地质构造和构造结构的资料的概括来确定矿床的位置)和成因法(适用于作为地层剖面一部分并反映沉积过程的沉积矿物)。今天,预测图更受欢迎,因为与成矿图不同,预测图反映的是对可能但尚未发现的含矿区和矿床的结论,以及它们的长期评估,通常还包括它们的种类和序列的描述。事实上,预报图不是一张图,而是一组附有相应说明的图。
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