Halloysite in late pleistocene rhyolitic tephra beds near Opotiki, coastal Bay of Plenty, North Island, New Zealand
Keyword(s):
Investigation of the clay mineralogy of 14 rhyolitic tephra beds with a suggested age of 125000 to 220000 years revealed that the squat cylindrical form of halloysite is the dominant crystalline mineral. This mineral has probably crystallized from allophane over a long time period, excess silica being precipitated as a weakly hydrated phase. The squat cylindrical crystals perhaps characterize halloysite formation in rhyolitic tephras.
1976 ◽
Vol 19
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pp. 179-187
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2015 ◽
Vol 144
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pp. 820-828
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1977 ◽
Vol 20
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pp. 905-917
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2009 ◽
Vol 90
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pp. 1095-1104
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1977 ◽
Vol 33
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pp. 34-39
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1983 ◽
Vol 29
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pp. 555-559
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