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Low-potash dacite drift pumice from the Coral Sea

Published online by Cambridge University Press:  01 May 2009

W. B. Bryan
Affiliation:
Geophysical Laboratory, Carnegie Institution, 2801 Upton Street, N.W., Washington D.C. 20008.

Summary

Drift pumice collected in December, 1964, from the Herald Cays in the western Coral Sea is chemically and petrographically a dacite, unusually low in K2O and with very calcic plagioclase. It is apparently identical to pumice washed ashore in Fiji in March, 1965; both collections are divisible into light and dark varieties on megascopic, optical and chemical criteria. This pumice is distinguishable from the widely distributed pumice of the 1962 South Sandwich eruption; it is considered to have originated along the Tonga-Kermadec ridge on the basis of available seismic and compositional data.

Type
Articles
Copyright
Copyright © Cambridge University Press 1968

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References

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