Paper No. 62
Presentation Time: 12:15 AM


WACKETT, Adrian, Department of Geosciences, Trinity University, One Trinity Place, San Antonio, TX 78212 and SMITH, Diane R., Department of Geosciences, Trinity University, One Trinity Place, Trinity University, San Antonio, TX 78212,

Mixing between basaltic and dacitic magmas has been invoked as an important process in the magmatic system of Mount St. Helens (MSH) (e.g. Gardner et al., 1995, Geology 23:523-526 and references therein). Bulk-rock major and trace element and isotopic studies of MSH andesites suggest they were generated by magma mixing; however, many MSH andesites do not exhibit mineralogical or textural features that clearly demonstrate mingling/mixing of different magma types. MSH tephra-fall layer Xb is an andesitic deposit erupted in the 16th century, which has been noted to contain dacite as clots and bands in the scoria (Mullineaux, 1996, USGS Prof. Paper 1563 and references therein). We used electron microprobe (EMP) and scanning electron microscope methods to analyze abundances of major elements in Xb glass. In each individual lapillus analyzed so far, SiO2 continuously varies from ~60 to 71 wt %, with concomitant variations in FeO, MgO, Al2O3, TiO2, CaO, and K2O. In one lapillus, glass with ~76 to 78 wt % SiO2 has also been identified. In that sample, an analytical traverse reveals a break in silica (between ~67-71 and 76-78 wt %) that occurs at a boundary < 50 microns wide separating glasses with different colors and vesicle morphologies. In other lapilli, bifurcating trends in FeO, MgO and TiO2 vs. SiO2 suggest the involvement of three endmembers in magma mingling processes. Coexisting magnetite and ilmenite occurring as microphenocrysts (~10 to 50 microns) in Xb glass were also analyzed with the EMP in order to estimate temperature and oxygen fugacity via geothermobarometry. Within individual lapilli, temperatures and oxygen fugacities span a range of ~200°C and ~3 log units, respectively. In one lapillus, Fe-Ti oxides coexisting with the highest SiO2 glass record the lowest temperatures, whereas Fe-Ti oxides in lower SiO2 glass record systematically higher temperatures. However, other lapilli show no clear relationship between temperature and glass chemistry. The glass chemistry and T-ƒO2 estimates for Xb samples suggest that micro-scale magma mingling processes were “caught in the act” via explosive eruption and rapid quenching, before blending or homogenization of hybrid magma was complete.