Dissertation, Rheinisch-Westfälische Technische Hochschule Aachen, 2020; Aachen 1 Online-Ressource (XVIII, 204, c Seiten) : Illustrationen, Diagramme, Karten (2020). = Dissertation, Rheinisch-Westfälische Technische Hochschule Aachen, 2020, Worldwide 120 deposits of critical metals (REE-Nb-Zr) are known which are hosted by alkaline igneous rocks. Some of these deposits were target for academic research and exploration campaigns since the last decades. The high diversity regarding lithologies and textures are two major features of this deposit type. This fact is well-founded by the also complex formation of the rocks which includes multiple stages of magmatic, othomagmatic and post-magmatic hydrothermal processes. As consequence, this complexity is also reflected by post-magmatic ore minerals like zircon, elpidite, bastnaesite and allanite which often features an intricate intergrowth with the gangue. Further, fine to very fine grain size can be observed among the ore minerals. These two typical properties hampering the economic use of this deposit type by a tremendous increase in expenditures regarding exploitation and beneficiation of the ore. In addition, the economical use is impeded by low ore grades (< 1 wt.%) and small total ore volumes. One big advantage of this deposit type, however, is the polymineralic character of the ore causes separation of HREE and LREE into different types of ore minerals which can be separated in mineral processing. Very often an increase in HREE/LREE ratios can be observe due to higher abundance of the more valuable HREE. This fact is often ignored by common deposit assessments using classic values as ore grade and tonnage for evaluation because REE content, for instance, is often reported only as the total sum of the REE. The geometallurgical assessment includes the evaluation of properties like elemental deportment, textures and liberation size of the individual ore minerals and thereby delivers more reliable data for the economic assessment. This study is focused on the Khalzan Buregtei alkali complex situated in western Mongolia as an example for the definition of geometallurgical attributes which can be used for the quantitative description of textural and mineralogical properties of alkaline rocks making them amenable to mineral processing. The outcropping part of the deposit and 3 drill cores were inspected and sampled in detail during two field campaigns. The samples were studies in detail using geochemical, petrographical and image analytical methods like SEM-bases QEMSCAN analysis. The detailed mineralogical investigations were able to identify the post-magmatic processes as key mechanisms for the formation of the ore mineral assemblage found today in the mineralized part of the studied complex. Diversification of mineralogical composition and rock textures observed ongoing to the ore formation were recorded quantitatively and were further evaluated for their use regarding the creation of optimized beneficiation schemes. It was figured out, that fine grained (< 45 µm) ore minerals were concentrated in close association to other secondary minerals like hematite, quartz and fluorite by the post-magmatic processes into pseudomorphic replacements of former magmatic minerals. This preserves magmatic textures as shape as well as the coarser grain size of the magmatic precurser (1000 µm). By this it is possible to distinguish this ore aggregates mineralogically and texturally from the barren rock. For example, separation of ore aggregates could be achieved using the magnetic properties assumed from the associated hematite on coarser grain size level. The quantitative records of these properties are used for forecasting the behaviour of individual ore minerals downstream the processing chain. By this, geometallurgical attributes like mineral association, texture of ore minerals and the elemental deportment are discussed and used for the creation of a beneficiation scheme optimized for the extraction of HFSE bearing ore minerals from alkali granitoid rocks. Further, geometallurgical domains are defined based on elemental deportment data to evaluate the entire deposit. The developed key parameters are finally discussed for their transferability for the geometallurgical assessment of other deposits of the same type. Therefore, fundamental properties of selected deposits were obtained from literature data., Published by Aachen