ISSN:
1432-0819
Keywords:
Key words Explosive volcanism
;
Magmatic
;
Phreatomagmatic
;
Crater Hill
;
Basalt
Source:
Springer Online Journal Archives 1860-2000
Topics:
Geosciences
Notes:
Abstract A series of alternating phreatomagmatic ("wet") and magmatic ("dry") basaltic pyroclastic deposits forming the Crater Hill tuff ring in New Zealand contains one unit (M1) which can only be interpreted as the products of mixing of ejecta from simultaneous wet and dry explosions at different portions of a multiple vent system. The principal characteristics of M1 are (a) rapid lateral changes in the thicknesses of, and proportions in juvenile components in individual beds, and (b) wide ranges of juvenile clast densities in every sample. M1 appears to have been associated with an elongate source of highly variable and fluctuating magma : water ratios and magma discharge rates. This contrasts with the only other documented mixed (wet and dry) basaltic pyroclastic deposits where mixing from two point sources of quite different but stable character has been inferred.
Type of Medium:
Electronic Resource
URL:
http://dx.doi.org/10.1007/s004450050126
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