Kaolinite, illite and quartz dissolution in the karstification of Paleozoic sandstones of the Furnas Formation, Paraná Basin, Southern Brazil

• Published in: Journal of South American earth sciences Vol. 63; pp. 20 - 35
• Main Authors: Melo, Mário Sérgio de, Guimarães, Gilson Burigo, Chinelatto, Adilson Luiz, Giannini, Paulo César Fonseca, Pontes, Henrique Simão, Chinelatto, Adriana Scoton Antonio, Atencio, Daniel
• Format: Journal Article
• Language: English
• Published: Elsevier Ltd 01-11-2015
• Subjects: Arenisation; Furnas Formation; Kaolinite dissolution; Non-carbonate karst; Quartz dissolution; Quartz dissolution; Non-carbonate karst; Kaolinite dissolution; Arenisation; Furnas Formation
• ISSN: 0895-9811; 1873-0647
• DOI: 10.1016/j.jsames.2015.06.011

Karstification processes in sandstones of the Furnas Formation, Silurian to Devonian of the Paraná Basin, have been described since the mid-twentieth century. However, some geologists still doubt the idea of true karst in sandstones. Studies carried out in the Campos Gerais region, Paraná State, Southern Brazil, aimed at investigating the nature of erosion processes in Furnas Formation and the role of the dissolution in the development of their notorious erosive features and underground cavities. These studies have led to the recognition of dissolution macro to micro features (‘furnas’, caves, ponds, sinks, ruiniform relief on cliffs and rocky surfaces, grain corrosion, speleothems, mineral reprecipitation and incrustation). The analysis (scanning electron microscopy, energy dispersive spectrometry and x-ray diffractometry) of sandstones and their alterites has indicated significant dissolution of clay cement along with discrete quartz grain dissolution. This mesodiagenetic cement (kaolinite and illite) is dissolved and reprecipitated as clay minerals with poorly developed crystallinity along with other minerals, such as variscite and minerals of the alunite supergroup, suggesting organic participation in the processes of dissolution and incrustation. The mineral reprecipitation usually forms centimetric speleothems, found in cavities and sheltered rocky surfaces. The cement dissolution associated with other factors (fractures, wet weather, strong hydraulic gradient, antiquity of the landforms) leads to the rock arenisation, the underground erosion and the appearance of the karst features. Carbonate rocks in the basement may locally be increasing the karst forms in the overlying Furnas Formation. The recognition of the karst character of the Furnas Formation sandstones has important implications in the management of underground water resources (increasingly exploited in the region), in the use of the unique geological heritage and in the prevention of geo-environmental accidents resulting from underground erosion phenomena.
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•Dissolution processes in the Furnas Formation sandstones are important and widespread.•Dissolution and grain release are critical factors in the origin of the sandstones landforms.•Removal of kaolinite cement results in the arenisation of the sandstones.•Micro to macroforms in the sandstones show close relation with kaolinite mobilization.•The Furnas Formation can be considered as an example of non-carbonate karst.