Scandium Ore Occurrences in the Ancient Weathering Crust in the Nakyn Kimberlite Field of Yakutia

IF 0.8 4区 地球科学 Q3 GEOLOGY
P. A. Ignatov, R. U. Eremenko, A. V. Tolstov, I. M. Ovchinnikov
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Abstract

In the Malo-Botuobinsky, Sredne-Markhinsky, and Ygyattinsky diamond-bearing areas of the Western Yakutian kimberlite province, the prerequisites and signs of scandium deposits in ancient weathering crusts overlying Lower Paleozoic rocks and associated with zones of ancient reservoir and soil oxidation. According to X-ray fluorescence and ICP MS analyses, in the Nakyn kimberlite field of the Sredne-Markhinsky diamond-bearing region, promising ore occurrences and scandium concentration halos have been established in clay deposits of redeposited weathering crusts of the Dyakhtar Formation of Late Triassic–Early Jurassic age. They are confined to the erosional surface of Lower Paleozoic carbonate rocks and Middle Paleozoic traps, with monzonite porphyries and kimberlites cutting through them, covered on top by a sedimentary cover of Jurassic terrigenous deposits. Concentration anomalies of scandium in clays of the Dyakhtar Formation are localized mainly in deluvial clay deposits of paleowatersheds and gravitate to the intersections of tectonic disturbances. The depth of their occurrence does not exceed 100 m, which is quite favorable for the extraction of scandium by borehole in situ leaching. Concentrations of scandium were detected at one of the sites before 262 g/t in Late Triassic weathering crust, including material from a Middle Paleozoic gabbro dike, as well as overlying colluvial clays of the Dyakhtar formations with a maximum of 462 g/t.

Abstract Image

雅库特纳金金伯利岩场古风化壳中的钪矿点
摘要 在西雅库特金伯利岩省的 Malo-Botuobinsky、Sredne-Markhinsky 和 Ygyattinsky 金刚石含矿区,下古生界岩石上覆盖的古风化壳中存在钪矿床的先决条件和迹象,并与古储层和土壤氧化带有关。根据 X 射线荧光和 ICP MS 分析,在 Sredne-Markhinsky 金刚石矿区的 Nakyn 金伯利岩矿区,晚三叠世-早侏罗世时期的 Dyakhtar Formation 重新沉积的风化壳粘土矿床中发现了有前景的矿点和钪富集晕。它们局限于下古生界碳酸盐岩和中古生界捕虏岩的侵蚀面,有单斜斑岩和金伯利岩穿过,上面覆盖着侏罗纪土沉积层。Dyakhtar 地层粘土中的钪浓度异常主要集中在古流域的冲积粘土沉积物中,并集中在构造扰动的交汇处。它们出现的深度不超过 100 米,这非常有利于通过钻孔原位浸取法提取钪。在其中一个地点的晚三叠世风化壳(包括来自中古生代辉长岩堤的物质)中检测到的钪浓度为 262 克/吨,在 Dyakhtar 地层的上覆胶结粘土中检测到的钪浓度最高,为 462 克/吨。
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来源期刊
Geology of Ore Deposits
Geology of Ore Deposits 地学-地质学
CiteScore
1.10
自引率
14.30%
发文量
24
审稿时长
6-12 weeks
期刊介绍: Geology of Ore Deposits is a periodical covering the topic of metallic and nonmetallic mineral deposits, their formation conditions, and spatial and temporal distribution. The journal publishes original scientific articles and reviews on a wide range of problems in theoretical and applied geology. The journal focuses on the following problems: deep geological structure and geodynamic environment of ore formation; distribution pattern of metallogenic zones and mineral deposits; geology and formation environment of large and unique metallic and nonmetallic deposits; mineralogy of metallic and nonmetallic deposits; physicochemical and isotopic characteristics and geochemical environment of ore deposition; evolution of ore-forming systems; radiogeology and radioecology, economic problems in exploring, developing, and mining of ore commodities.
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