Comparative geothermometry of recent Hawaiian eruptions

Autor: Norman G. Banks, Christina Heliker, Christina A. Neal, Rosalind Tuthill Helz, Edward W. Wolfe
Rok vydání: 1995
Předmět:
Zdroj: Journal of Geophysical Research: Solid Earth. 100:17637-17657
ISSN: 0148-0227
1983-1986
DOI: 10.1029/95jb01309
Popis: In this paper we compare lava temperatures measured using Cr-A1 thermocouples or infrared spectrometry with estimated quenching temperatures based on the glass geothermometry calibration of Helz and Thornber (1987). Comparative data are available for the April 1982 and September 1982 summit eruptions, the Pu'u 'O'o east rift eruption (1983-1986), all three eruptions at Kilauea, and the 1984 Mauna Loa eruption. The results show that quenching temperatures, based on the MgO contents of Kilauean glasses (TMgo) , lie within _+ 10oC of field measurements using the infrared spectrometer for 85% of the samples. Where a Cr-A1 thermocouple was used, 90% of the field measurements lie within +1 o to -11oC of TMg o for samples with Tfiel d > 1130oC. Samples where Tfiel d < 1130oC show larger divergence. The uncertainty in TMg o by itself is _+ 10oC, so the level of agreement between field measurements and TMg o is very good for Kilauean lavas. Systematic comparison of field measurements of temperature with glass geothermometry for the 1984 Mauna Loa eruption suggests that, although the field and glass temperatures lie within + 10oC of each other, the Kilauean TMg o calibration is nevertheless not appropriate for Mauna Loa glasses and that actual quenching temperatures for Mauna Loa samples will lie 10o-20oC higher than would be predicted from the Kilauea calibration curve. Consideration of possible effects of variable volatile content suggest that in most cases these are small. Samples erupted early in an eruption may reflect preeruptive water contents different enough to affect TMg o significantly, but later spatter samples and all flow samples appear to have equilibrated at low enough water contents for the calibration to be applicable. We conclude that the MgO-based geothermometer can be applied to glassy Kilauean samples to give temperatures that generally will lie within _+ 10oC of a field measurement. Plots of glass MgO content versus time, if a suitable sample base is available, should give a thorough, quantitative record of the thermal history of any Kilauean eruption.
Databáze: OpenAIRE
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