Produção Nacional
Revisado por pares
Giant-geode endowment of tumuli in the Veia Alta flow, Ametista do Sul
2017; Elsevier BV; Volume: 77; Linguagem: Inglês
10.1016/j.jsames.2017.04.013
ISSN1873-0647
AutoresLéo Afrâneo Hartmann, Juliana Pertille, Lauren da Cunha Duarte,
Tópico(s)Geography and Environmental Studies
ResumoTumuli are a common feature of pahoehoe basaltic flows, interspersed with pits, and furnished the necessary volume of rock in the Paraná volcanic province for hydrothermal alteration and ballooning to form large cavities (1–2 m common). Filling by amethyst and other minerals resulted in the largest world deposit of geodes, Ametista do Sul. The flat-lying fracture positioned 1 m below the 2–3 m thick geodic level crosses the plateau and is a major guide for exploration and gallery opening. The geodes are limited on the top by the platy joint layer, which is covered by an auto-breccia with undulating lower limit. This wave mimicks and is internal to the structure of tumuli and pits at the surface. This field-oriented survey of galleries selected out of 300 active mines resulted in the description of the internal structure of the remarkable Veia Alta pahoehoe flow, in addition to observations in Uruguay.
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