The importance of clay minerals for stratigraphic and paleogeographic reconstructions of diamond-promising territories
DOI:
https://doi.org/10.17308/geology/1609-0691/2026/1/43-57Keywords:
argillaceous minerals, sedimentary formations, sedimentogenesis, diagenesis, metagenesis of sedimentsAbstract
Introduction: the characteristics of clay minerals in sedimentary rocks are determined by the nature of the source areas, the influence of the hydrochemical nature of the environment on the material entering sedimentation areas, and the scale of changes in the chemical composition and properties of the material depending on the intensity of post-sedimentation transformation of deposits. These factors contribute to the development of a sequential process of aggradational alteration of primary allochthonous clay material in all lithological types of rocks. The formation of authigenic clay formations occurs in the pores of sandstone-siltstone rocks and along the fractures of carbonate and terrigenous-carbonate rocks.
Objects, Research Methodology, Results and Their Interpretation: a brief analysis of the behaviour of clay minerals in sedimentary formations at various stages of sedimentogenesis, diagenesis, catagenesis and metagenesis has been carried out. It is shown that each of the zones identified in the Earth’s crust is characterised by different combinations of clay minerals and degrees of post-sedimentation rock transformation. Clay minerals and their associations in terrigenous, terrigenous-carbonate, carbonate, volcanic and halogenic formations have been characterised. Clay minerals from the early stages of sedimentation and diagenesis (partially catagenesis) have been described in particular detail. These stages are usually associated with most ancient (Upper Palaeozoic and Mesozoic) diamond-bearing placers. The presence of indicator minerals of kimberlites in such placers is commonly used to prospect for primary diamond deposits using the heavy-mineral concentrate (placer) mineralogical method.
Using specific diamond-bearing areas of the Siberian Platform (SP) as an example, the importance of studying the material composition of volcanic formations and the distribution patterns of their material during the formation of multi-age diamond reservoirs has been demonstrated for solving predictive and prospecting tasks.
Conclusion: based on the study of deposits from terrigenous, terrigenous-carbonate, carbonate and volcanic formations - where clay minerals are noted to be of both authigenic and allochthonous origin - the widespread development of structurally imperfect varieties has been demonstrated. The latter are characterised by significant defects (i.e., vacancies in the structure) that are not fully filled even up to the metagenesis stage (MS). This is due to the fact that formation waters and pore solutions at the lithogenesis stages preceding MS retain a deficit of the major cations essential for the structures of layered silicates. This leads to relatively minor changes in the material of reworked weathering crusts during their transport into sedimentary basins. This has been illustrated using the example of Upper Palaeozoic and Mesozoic sedimentary sequences from the main diamond-bearing regions of the SP.
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