Local Factors of the Formation of Coastal-Marine Rare Metal–Titanium Placers

IF 0.7 4区 地球科学 Q4 GEOCHEMISTRY & GEOPHYSICS
A. V. Lalomov
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Abstract

Local factors of the formation of coastal-marine rare metal–titanium placers were analyzed for creating the prospecting-oriented geological-dynamic model that allows to predict the prospects of rare metal–titanium placer mineralization. Their influence on the structure, composition, localization of placer concentrations within sedimentation basins, and dynamic interaction during the formation of productive sediments was investigated. Based on the works of previous researchers devoted to the historical-geological and regional tectonic factors controlling the formation of these placers, we developed a qualitative model of the formation of placer concentrations in different rank areas (districts, clusters, fields, and specified placer bodies), which can serve as a basis for the creation of prospecting-orientated model of the deposit and planning the exploration and evaluation work. Among the factors controlling the formation of placers, we can identify: hydrodynamic processes characterizing the types and mechanisms of placer concentrations (littoral and sublittoral) within the dynamically active coastal zone; lithodynamic processes depending on the abrasion-accumulative setting of the coast and parameters of the alongshore sediment flow; structural-dynamic processes controlling the formation of economically significant productive deposits and their localization; and the transgressive-regressive setting of a basin that determines the structure of placer bodies and their transformation at the postsedimentary stage. Large economically significant rare metal–titanium placer deposits are only formed under conditions of a joint realization of the positive potential of these factors. The developed qualitative model can serve as a basis for digitizing the forecasting of rare metal–titanium placer mineralization.

Abstract Image

海岸-海洋稀有金属-钛砂形成的局部因素
分析了海岸-海相稀有金属-钛砂矿形成的局部因素,建立了以找矿为导向的稀有金属-钛砂矿成矿前景地质动力学模型。研究了它们对沉积盆地的结构、组成、砂浓度的局部化以及生产沉积物形成过程中的动态相互作用的影响。在前人研究历史地质因素和区域构造因素控制砂矿形成的基础上,建立了不同等级区域(区、团、田、特定砂体)砂矿集中形成的定性模型,为建立找矿模式和规划找矿评价工作提供依据。在控制砂矿形成的因素中,我们可以确定:在动力活跃的海岸带内,表征砂矿(滨海和亚滨海)浓度类型和机制的水动力过程;岩石动力学过程取决于海岸的磨积环境和沿岸沉积物流动参数;控制具有经济意义的生产性矿床形成及其定位的构造动力过程;盆地的海侵退背景决定了砂体的构造及其沉积后阶段的转化。具有重要经济意义的大型稀有金属-钛砂矿只有在这些因素的积极潜力共同发挥的条件下才能形成。所建立的定性模型可作为稀有金属-钛砂矿化数字化预测的基础。
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来源期刊
Lithology and Mineral Resources
Lithology and Mineral Resources 地学-地球化学与地球物理
CiteScore
1.30
自引率
37.50%
发文量
29
审稿时长
>12 weeks
期刊介绍: Lithology and Mineral Resources is an international peer reviewed journal that publishes articles on a wide range of problems related to the formation of sedimentary rocks and ores. Special attention is given to comparison of ancient sedimentary rock and ore formation with present-day processes. The major part of the journal is devoted to comparative analysis of sedimentary processes on the continents and in oceans, as well as the genetic aspects of the formation of sedimentary and hydrothermal–sedimentary mineral resources. The journal welcomes manuscripts from all countries in the English or Russian language.
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