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. © 1952 Nature Publishing Group.
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CITATION STYLE
APA
McDowall, I., & Vose, W. (1952). Sedimentation of halloysite. Nature, 170(4322), 368. https://doi.org/10.1038/170368a0
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