Storage conditions of Bezymianny Volcano parental magmas: results of phase equilibria experiments at 100 and 700 MPa

• Published in: Contributions to mineralogy and petrology 2013-11, Vol.166 (5), p.1389-1414
• Main Authors: Almeev, Renat R., Holtz, Francois, Ariskin, Alexei A., Kimura, Jun-Ichi
• Format: Article
• Language: English
• Subjects: Analysis; Crystallization; Degassing; Earth and Environmental Science; Earth Sciences; Fractionation; Geochemistry; Geology; Magma; Magnetite; Mineral Resources; Mineralogy; Original Paper; Petrology; Product development; Volcanoes
• ISSN: 0010-7999; 1432-0967
• DOI: 10.1007/s00410-013-0934-x

The crystallization sequence of a basaltic andesite from Bezymianny Volcano, Kamchatka, Russia, was simulated experimentally at 100 and 700 MPa at various water activities ( a H 2 O) to investigate the compositional evolution of residual liquids. The temperature ( T ) range of the experiments was 950–1,150 °C, a H 2 O varied between 0.1 and 1, and the log of oxygen fugacity ( f O 2 ) varied between quartz–fayalite–magnetite (QFM) and QFM + 4.1. The comparison of the experimentally produced liquids and natural samples was used to constrain the pressure (P) – T – a H 2 O– f O 2 conditions of the Bezymianny parental magma in the intra-crustal magma plumbing system. The phase equilibria constraints suggest that parental basaltic andesite magmas should contain ~2–2.5 wt% H 2 O; they can be stored in upper crustal levels at a depth of ~15 km, and at this depth they start to crystallize at ~1,110 °C. The subsequent chemical evolution of this parental magma most probably proceeded as decompressional crystallization occurred during magma ascent. The final depths at which crystallization products accumulated prior to eruption are not well constrained experimentally but should not be shallower than 3–4 km because amphibole is present in natural magmas (>150 MPa). Thus, the major volume of Bezymianny andesites was produced in a mid-crustal magma chamber as a result of decompressional crystallization of parental basaltic andesites, accompanied by mixing with silicic products from the earlier stages of magma fractionation. In addition, these processes are complicated by the release of volatiles due to magma degassing, which occurs at various stages during magma ascent.