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Location: 365 km S from Teresina, Brazil
Unnamed RdCapitão Gervásio OliveiraBrazil64763-000
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The PNP deposit is a nickel-cobalt laterite deposit.The geological setting of the Piaui deposit is within a terrain of intensely deformed volcanic, volcanosedimentary and sedimentary rocks of Precambrian age which have been intruded by mahc-ultramafic bodies. The Piaui ultramafic comprises a massive body of serpentinised dunite and peridotite, grading to the south into a mafic complex of diorites, gabbros and troctolites. The ulnamafic body as expressed by the lateritised hill is about 3 km long (E-W) by about 1.3 km wide (N-S). The hill rises about 100 m above the surrounding plain. The ultramahc body has been intensely and deeply lateritised forming the nickel deposit. The character of the nickeliferous laterite is typical of lateritised dunites, which are composed almost entirely of MgO and SiOz and are highly susceptible to breakdown in the weathering environment. Olivine breaks down as Mg is rapidly removed in solution, and the relatively small amount of Fe remains as limonite.In the study region, two types of rocks are found: sedimentary in the north, metamorphic and crystalline in the south. Sedimentary rocks, due to the physical characteristics of permeability (ability to let liquids pass through the interior without altering it), are able to store underground water and form aquifers. Metamorphic rocks, as the name implies (Greek: meta = change; morphs = shape) are those that have undergone transformations during their formation. These changes involved exposure to different temperatures and pressure for a long time and therefore took on a different shape and mineral composition than the initial rock. This type of rock attracts economic interest, such as the Piaui Nickel Project.
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