Abstract
IN the North Auckland peninsula of New Zealand there are extensive deposits of halloysitic clays formed by weathering of dacite. Attempts to determine the particle-size distribution of a well-crystallized sample from Matauri Bay, Whakarara Survey District, have revealed anomalous sedimentation behaviour.
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McDOWALL, I., VOSE, W. Sedimentation of Halloysite. Nature 170, 368 (1952). https://doi.org/10.1038/170368a0
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DOI: https://doi.org/10.1038/170368a0
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