Advances in Geophysics Applied to the Search for Banded Iron Formation-Related, High-Grade Hematite Iron Ore

Author(s):  
Marcus Flis
2008 ◽  
Author(s):  
Steffen Hagemann ◽  
Carlos Alberto Rosière ◽  
Jens Gutzmer ◽  
Nicolas J. Beukes

2020 ◽  
Vol 10 (1) ◽  
Author(s):  
Andrey O. Kalashnikov ◽  
Ivan I. Nikulin ◽  
Dmitry G. Stepenshchikov

Abstract We stated and solved three successive problems concerning automatization of geological mapping using the case of the Bolshetroitskoe high-grade iron ore deposit in weathered crust of Banded Iron Formation (Kursk Magnetic Anomaly, Belgorod Region, Russia). (1) Selecting a classification (clustering) method of geochemical data without reference sampling, i.e., solution of an “unsupervised clustering task”. We developed 5 rock classifications based on different principles, i.e., classification by visual description, by distribution of economic component (Fe2O3), by cluster analysis of raw data and centered log-ratio transformation of the raw data, and by artificial neural network (Kohonnen’s self-organized map). (2) Non-parametric comparison of quality of the classifications and revealing the best one. (3) Automatic 3D geological mapping in accordance with the best classification. The developed approach of automatic 3D geological mapping seems to be rather simple and plausible.


2017 ◽  
Vol 296 ◽  
pp. 62-77 ◽  
Author(s):  
Mathias S. Egglseder ◽  
Alexander R. Cruden ◽  
Hilke J. Dalstra ◽  
Leigh Nicholas

Author(s):  
Lydia Maria Lobato ◽  
E Silva Figueiredo Rosaline Cristina ◽  
Steffen Hagemann ◽  
Warren Thorne ◽  
Márcia Zucchetti

2015 ◽  
Vol 45 (2) ◽  
pp. 193-216 ◽  
Author(s):  
Lucilia Aparecida Ramos de Oliveira ◽  
Carlos Alberto Rosière ◽  
Francisco Javier Rios ◽  
Sandra Andrade ◽  
Renato de Moraes

<p>Chemical signatures of iron oxides from dolomitic itabirite and high-grade iron ore from the Esperança deposit, located in the Quadrilátero Ferrífero, indicate that polycyclic processes involving changing of chemical and redox conditions are responsible for the iron enrichment on Cauê Formation from Minas Supergroup. Variations of Mn, Mg and Sr content in different generations of iron oxides from dolomitic itabirite, high-grade iron ore and syn-mineralization quartz-carbonate-hematite veins denote the close relationship between high-grade iron ore formation and carbonate alteration. This indicates that dolomitic itabirite is the main precursor of the iron ore in that deposit. Long-lasting percolation of hydrothermal fluids and shifts in the redox conditions have contributed to changes in the Y/Ho ratio, light/heavy rare earth elements ratio and Ce anomaly with successive iron oxide generations (martite-granular hematite), as well as lower abundance of trace elements including rare earth elements in the younger specularite generations.</p>


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