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- W1966289786 abstract "Abstract Aluminous laterites which occur above basalts of Plio-Pleistocene age in the Kerikeri area of North Auckland have been formed by processes initiated in the late Pliocene and continuing during the interglacial periods. Initial alteration leached the parental basalt of alkalis and about half its silica to produce a saprolite composed of halloysite, amorphous to subcrystalline iron oxides and oxyhydroxides, and relict magnetite and ilmenite. Continued leaching removed further silica from halloysite to yield gibbsite while dehydration of the upper layers aided crystallisation of the iron oxyhydroxides. Resilicification appears to have occurred at one locality." @default.
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- W1966289786 date "1980-09-01" @default.
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- W1966289786 title "The chemical and mineralogical changes accompanying the laterization of basalt at Kerikeri, North Auckland" @default.
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- W1966289786 doi "https://doi.org/10.1080/03036758.1980.10415331" @default.
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