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It is undoubtable that the geological path followed by a bentonite natural occurrence, will set a birthmark in terms of grade and quality, the former being expressed in terms of mineralogical composition, smectite content and other aspects derived from the bulk sample characterization, and the latter being expressed in terms of the crystal chemistry of smectite species present and derived from the clay size fraction observations. The influence of parent rock composition, genesis mode, burial history and preservation conditions after alteration, would set the fingerprint on bentonite and inherent structural features in smectites species, which determines potential industrial and scientific uses. The following thesis aims to evaluate physicochemical properties of 12 bentonite samples, coming from the six most relevant bentonite bearing geological areas located in the Mercosur economic block (Argentina, Brazil and Uruguay); in order to stablish possible correlations between distinctive geological contexts, and observed characteristics from whole rock providing information regarding grade and the clay size fraction will provide information regarding quality. Mineralogical composition corroborated the tendency to be influenced by the geochemical signature of parent rock firstly, and secondly genesis mode (probably due to lack of information in this aspect). Age, on the other hand, could on the contrary, be a misleading parameter; in the sense that preservation is not necessarily time dependent. Poor grade and the presence of mixed layers and accessory clay mineral phases (mostly kaolinite but also I/S, illite and pyrophyllite) appear to be associated with hydrothermal to sedimentary alteration modes, higher grade bentonites with tendency to yield extreme relative values of physical properties, measured in layer charge, swelling and organic sorption, were found in association to diagenetic bentonites. In terms of smectite species, all members found belong to the montmorillonite-beidellite series, and rhyolitic to dacitic volcanic source, tends to alter into the 1 Paraguay and Venezuela are also members of the Mercosur Economic trade block, but do not report Bentonite mining activity.

Correlations between geological track and bentonite quality in the mercosur trade block.