JpGU-AGU Joint Meeting 2020

Presentation information

[E] Poster

S (Solid Earth Sciences ) » S-VC Volcanology

[S-VC42] Dynamics of volcanic eruptions and their physical and chemical processes

convener:Atsuko Namiki(Graduate School of Integrated Arts and Sciences, Hiroshima University), Christian Huber(Brown University), Michael Manga(University of California Berkeley), Yujiro Suzuki(Earthquake Research Institute, The University of Tokyo)

[SVC42-P14] Intermittent ascent of aphyric andesitic melts revealed by cryptic micro-antecryst textures

*Charline Lormand1, Georg F Zellmer1, Naoya Sakamoto2, Geoff Kilgour3, Teresa Ubide4, Hisayoshi Yurimoto2, Alan Palmer5, Karoly Nemeth1, Yoshiyuki Iizuka6, Anja Moebis5 (1.School of Agriculture and Environment, Volcanic Risk Solutions, Massey University, PO Box 11222, Palmerston North 4442, New Zealand, 2.Isotope Imaging Laboratory, Natural History Sciences, Hokkaido University, Sapporo 060-0810, Japan, 3.GNS Science, Wairakei Research Centre, Private Bag 2000, Taupo 3352, New Zealand, 4.School of Earth and Environmental Sciences, The University of Queensland, Brisbane, QLD 4072, Australia , 5.School of Agriculture and Environment, Department of Soil Science, Massey University, PO Box 11222, Palmerston North 4442, New Zealand , 6.Institute of Earth Sciences, Academia Sinica, 128 Academia Road Sec. 2, Nankang, Taipei 11529, Taiwan)

Keywords:microlites, micro-phenocrysts, zonations, Tongariro Volcanic Centre, magma ascent

Crystal cargoes transported by arc magmas upon eruption often consist of complexly zoned phenocrysts with diverse histories. While these crystals record the early stage of magma formation and evolution, they are not ideal recorders of ascent processes, which are the keys to useful constraints for adequate volcano monitoring. Conversely, microlites and micro-phenocrysts, frequently associated with decompression-induced degassing or cooling, are relevant recorders of late-stage ascent processes. Our study focusses on the active Tongariro Volcanic Centre (TgVC), located at the southern end of the Taupo Volcanic Zone; an active volcanic complex that has produced a wide range of explosive eruption styles fed by intermediate magmas. Scoriae from these volcanoes contain glassy and nearly-aphyric tephras, carrying microlites of plagioclase and pyroxene (mostly orthopyroxene). Major element analyses, combined with textural information, are used to assess equilibrium between the microlites/micro-phenocrysts and the groundmass glass. Chemical disequilibrium of some plagioclase and pyroxene crystals with the surrounding glass is common in most tephras. To investigate this further, we mapped plagioclase and pyroxene phenocrysts, micro-phenocrysts and microlites at submicron resolution for major and trace element distributions via chemical mapping and SIMS-SCAPS imaging. From a total of 105 images, six plagioclase textural patterns are noted: resorption and overgrowth, oscillatory zoning, single compositional jump, sieve textures, fractures, and strontium zonation; while in pyroxene microlites the following textures are found: resorption and overgrowth, calcium-rich rims, magnesian core and calcic rims, fractures, and aluminium zonation. Microlite textures are observed down to <30 µm in most tephras from TgVC, and interpreted in the context of an interplay of magmatic processes involving multiple events of magma recharge/mixing, pressure fluctuations, fracturing, and rapid cooling and crystal growth. Since TgVC is located in an extensional tectonic setting, we envision a vertically oriented magma plumbing system, where short-lived and nearly-aphyric magma pulses accommodate crustal extension through dyking. Explosive eruptions occur when a hot magma batch fractures through previous intrusions, recycling a variety of small crystals grown under diverse physico-chemical conditions and stored in rapidly cooled, previously intruded dykes. Thus, textures cryptic to conventional imaging indicate that a significant proportion of the microlitic and micro-phenocrystic mineral cargo is of antecrystic origin (i.e. hence referred as “micro-antecrysts”) and cannot be attributed to late-stage nucleation and growth at the onset of volcanic eruptions.