JpGU-AGU Joint Meeting 2017

Presentation information

[JJ] Poster

S (Solid Earth Sciences) » S-VC Volcanology

[S-VC50] [JJ] Volcanic and igneous activities, and these long-term forecasting

Sat. May 20, 2017 3:30 PM - 5:00 PM Poster Hall (International Exhibition Hall HALL7)

convener:Teruki Oikawa(Institute of Earthquake and Volcano Geology, Geological Survey of Japan, National Institute of Advanced Industrial Science and Technology), Takeshi Hasegawa(Department of Earth Sciences, College of Science, Ibaraki University), Daisuke MIURA(Geosphere Sciences, Civil Engineering Research Laboratory, Central Research Institute of Electric Power Industry), Nobuo Geshi(Geological Survey of Japan, The National Institute of Advanced Industrial Science and Technology)

[SVC50-P16] Glaciovolcanic and magmatic evolution of Ruapehu volcano, New Zealand

*Chris Conway1, Colin Wilson2, John Gamble2, Graham Leonard3, Dougal Townsend3 (1.National Museum of Nature and Science, 2.Victoria University of Wellington, 3.GNS Science)

Keywords:lava-ice interaction, andesite petrogenesis, Ruapehu volcano

Chronostratigraphic studies of continental arc stratovolcanoes reveal the timing and types of past eruptive behaviour and are therefore crucial for constraining magma evolution models as well as the future eruption potential in these active settings. Such studies can be complicated by complex stratigraphic relationships caused by glaciovolcanism (eruptions in the presence of ice), glacial erosion and sector collapse for edifices that have been glaciated. These issues are relevant to the numerous high-altitude cones that define Earth’s continental volcanic arcs. A key example of this is Ruapehu, which is an active andesite-dacite stratovolcano located at the southern end of the Taupo Volcanic Zone, New Zealand. The growth of the Ruapehu edifice has occurred throughout coeval eruptive and glacial histories since ~200 ka. Here, new high-precision 40Ar/39Ar ages and whole-rock major and trace element data for Ruapehu lava flows are integrated with geological mapping and glacier reconstructions. The data provide a high-resolution chronostratigraphic and geochemical framework for investigating processes of ice-marginal lava flow emplacement and magma generation. In particular, the following concepts are addressed in this study: (1) the potential for ice-bounded lava flows to provide paleoclimate information; (2) the role of deglaciation in triggering Holocene sector collapses; (3) the variable extent of crustal assimilation in andesite-dacite magma genesis during the lifetime of a stratovolcano.