| Autor: |
Andres, RJ, Kyle, PR, Stokes, JB, Rose, WI |
| Zdroj: |
Bulletin of Volcanology; Dec1989, Vol. 52 Issue 2, p113-117, 5p |
| Abstrakt: |
An SO flux of 1170±400 (1σ) tonnes per day was measured with a correlation spectrometer (COSPEC) in October and November 1986 from the continuous, nonfountaining, basaltic East Rift Zone eruption (episode 48A) of Kilauea volcano. This flux is 5-27 times less than those of highfountaining episodes, 3-5 times greater than those of contemporaneous summit emissions or interphase Pu'u O'o emissions, and 1.3-2 times the emissions from Pu'u O'o alone during 48A. Calculations based on the SO emission rate resulted in a magma supply rate of 0.44 million m per day and a 0.042 wt% sulfur loss from the magma upon eruption. Both of these calculated parameters agree with determinations made previously by other methods. [ABSTRACT FROM AUTHOR] |
| Databáze: |
Complementary Index |
| Externí odkaz: |
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