Spatial Modeling of Occurrence Sites of Paleotocas in Serra do Gandarela and Curral, with a view to Prospecting Places Favorable to Existence and Other Discoveries in the Quadrilátero Ferrífero - MG
Spatial Modeling of Occurrence Sites of Paleotocas in Gandarela and Curral ranges, Quadrilátero Ferrífero - MG
DOI:
https://doi.org/10.5016/geociencias.v41i03.15963Abstract
The ferruginous geosystem of the Quadrilátero Ferrífero (QFe) constantly involves scenarios of dispute between mineral exploration and environmental conservation. Recent studies in caves in the region have confirmed that two of them are palaeoburrows. In ferruginous lithology, they were initially verified in the Vale do Rio Peixe Bravo, north of Minas Gerais. In the QFe, the only records found are located in Serra do Gandarela and Serra do Curral, excavated in the canga / saprolite contact. Especially the Gandarela paleotoca is threatened by mining. The objective of this work was to discriminate potential target areas of new occurrences of palaeoburrows in the QFe from the comparison of the geomorphological and geological characteristics of the areas of occurrence of these ichnofossils both in the QFe and in other ferruginous geosystems. The methodological procedures involved the Delphi technique and the use of geoprocessing in the construction of thematic maps and the elaboration of a map of potential occurrences. The analysis allowed to identify that the two paleotocas and most of the natural cavities registered in high potential zones, occur in rocks of the Itabira Group (itabirites). As they are areas of great interest to mining, they become a priority for investigation and characterization, in order to guarantee the integrity of possible paleontological records.
Key words: Palaeoburrows; Ichnofossils; Geoconservation; Geoprocessing; Delphi.