"' Silicate type "'( or saprolite type ) nickel ore formed beneath the limonite zone.
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Saprolite is not as weathered as laterite; there is a continuum from the upper layer of saprolite to laterite.
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Saprolite is not as weathered as laterite; there is a continuum from the upper layer of saprolite to laterite.
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Nickel content is higher in the saprolite zone although cobalt is an important by-product of the limonite horizon.
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Frequently, erosion has removed the layers of altered rock and other saprolite surrounding corestones that were produced by spheroidal weathering.
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Two types of nickel ore are of commercial importance, limonite ( oxide ) ore and saprolite ( nickel silicate ) ore.
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It includes igneous, metamorphic, and sedimentary geology; the main types of rocks in the area are gneiss, slate and saprolite.
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The Goro mine is targeted to produce about 40, 000 tonnes of nickel per year, and also some cobalt from saprolite deposits.
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Saprolite is a particular example of a residual soil formed from the transformation of granite, metamorphic and other types of bedrock into clay minerals.
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A layer of saprolite ( chemically weathered rock ) separates the Bailey Rock Rhyolite formation from the overlying Caldera-Fill Sequence-era rocks.
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