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Decompression experiments as an insight into ascent rates of silicic magmas.

Abstract : An experimental study of H2O exsolution, bubble growth and microlite crystallisation during ascent (decompression) of silicic magmas in the volcanic conduit is presented. Isobaric and decompression experiments were performed on a rhyolitic melt at 860 °C, NNO+1, H2O saturation, and pressures between 15 and 170 MPa. Two sets of decompression experiments were performed, with decompression rates varying between 0.001 and 960 MPa/min: (1) from 150 to 50 MPa (high-pressure decompression), and (2) from 50 to 15 MPa (low-pressure decompression). The experiments highlight incomplete H2O exsolution for decompression rates>100 MPa/min, incomplete bubble growth for decompression rates>0.1 MPa/min, crystal nucleation time lags, and incomplete chemical re-equilibration to final pressures. The observed crystallisation process, i.e. growth versus nucleation, depends on the decompression range. Indeed, decompression-induced crystallisation during high-pressure decompressions is dominated by growth of existing crystals, whereas during low-pressure decompressions crystal nucleation is the dominating process. This study provides a means to infer magma ascent rates in eruptions of silicic magmas through a combined petrologic and experimental approach.
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Submitted on : Friday, November 25, 2016 - 5:11:10 PM
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Caroline Martel, Burkhard C. Schmidt. Decompression experiments as an insight into ascent rates of silicic magmas.. Contributions to Mineralogy and Petrology, Springer Verlag, 2003, 144, pp.397-415. ⟨10.1007/s00410-002-0404-3⟩. ⟨hal-00069447⟩

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