Abstract
The densities of 800 rock samples representing the major sedimentary, metamorphic, and igneous formations in New Zealand are summarised and tabulated. The youngest Pleistocene rocks have a wet density of l-88g/cm3, and this increases down through the Tertiary column to 2-55g/cm3 in the Cretaceous. Jurassic-Permian greywackes have a wet density of 2-65g/cm3 and the oldest sediments a wet density of 2-68 g/cm3. Metamorphosed rocks have higher densities. The greatest anomaly in the igneous rock densities is the very low value (2-18g/cm3) for the rhyolites of the Rotorua thermal area. © Taylor & Francis Group, LLC.
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CITATION STYLE
Hatherton, T., & Leopard, A. E. (1964). The densities of New Zealand rocks. New Zealand Journal of Geology and Geophysics, 7(3), 605–625. https://doi.org/10.1080/00288306.1964.10422108
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