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(2020)
M.Yu., Main types and mineral composition of bauxites in Kursk Magnetic Anomaly
(2016)
Bauxites in the KMA
(1984)
Phanerozoic weathering crusts, associated rocks in the Voronezh anteclise, and nonmetallic mineral resources
Main types and mineral composition of bauxites in Kursk Magnetic Anom
(2013)
Berthierine—main silicate of high-grade iron ore deposits in the KMA, Vestn
(2014)
Morphology and formation conditions of the ferruginous weathering crust in the Belgorod area of KMA, Vestn
(2015)
Ferruginous weathering crusts in the Belgorod area of KMA, Trudy NII Geol. Voronezh
(2019)
Fossil organisms and traces of their vital activity in bauxites of the KMA, Vestn
(2015)
Types of hypergene high-grade iron ores in the Belgorod area of Kursk Magnetic Anomaly
(2013)
Berthierine-main silicate of high-grade iron ore deposits in the KMA
(1997)
Size effect and organic matter as factors controlling the evolution of mineral formation in the hypergenesis zone: Synchronous thermal analysis, Abstract of DSC (Geol
(2008)
Istoricheskaya minerageniya (Historical Minerageny)
S. Fritz, T. Toth (1997)
An Fe-Berthierine from a Cretaceous Laterite: Part II. Estimation of Eh, pH and pCO2 Conditions of FormationClays and Clay Minerals, 45
M. Ovchinnikova (2020)
The Main Types and Mineral Composition of Bauxites of the Kursk Magnetic Anomaly, 162
(1984)
Phanerozoic weathering crusts, associated rocks in the Voronezh anteclise, and nonmetallic mineral resources, Abstract of DSc (Geol.–Miner.) Dissertation, Voronezh: Voronezh
(2016)
Biomorphic textures in high-grade iron ores of the KMA based on results of the SEM study
(2015)
Ferruginous weathering crusts in the Belgorod area of KMA
(2015)
Types of hypergene high-grade iron ores in the Belgorod area of Kursk Magnetic Anomaly, Vestn
(2008)
Istoricheskaya minerageniya (Historical Minerageny), Voronezh: Voronezh
(1975)
Stages of the weathering crust formation in the Upper Proterozoic and Paleozoic in the Voronezh anteclise
D. Whitney, B. Evans (2010)
Abbreviations for names of rock-forming mineralsAmerican Mineralogist, 95
(2002)
Geologiya Voronezhskoi anteklizy (Geology of the Voronezh Anteclise), Voronezh: Voronezh
High-grade iron ores and bauxites of the Kursk magnetic anomaly (KMA) were formed in weathering crusts on the Early Precambrian ferruginous quartzites and shales, i.e., banded iron formation (BIF). Thus far, weathering crusts on the BIF were considered separately, although they formed simultaneously and represent a single sequence in each ore region. Therefore, it is of great interest to compare the coeval weathering crusts on rocks of the formation under consideration for a complex prediction of high-grade iron ores and bauxites. The obtained results showed that the BIF-hosted iron ores were formed during all stages of crust formation in the Paleozoic and such ores can be predicted throughout the KMA, whereas bauxites were only formed in inter-ore shales on the southwestern flank of the anomaly.
Lithology and Mineral Resources – Springer Journals
Published: Aug 1, 2022
Keywords: Kursk magnetic anomaly; weathering crusts; high-grade iron ores; bauxite; magnetite; martite; hematite; boehmite; gibbsite
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