Lithium and strontium isotopic systematics of waters around Ontake volcano, Japan: Implications for deep-seated fluids and earthquake swarms

Details Lithium and strontium isotopic systematics of waters around Ontake volcano, Japan: Implications for deep-seated fluids and earthquake swarms Lithium and strontium isotopic systematics of waters around Ontake volcano, Japan: Implications for deep-seated fluids and earthquake swarms

Sep 2010

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=2010e%26psl.297..567n&link_type=abstract

Earth and Planetary Science Letters, Volume 297, Issue 3-4, p. 567-576.

Computer Science

Scientific paper

Since 1976, earthquake swarms have occurred beneath the southeast flank of Ontake volcano in central Japan. Electrical conductivity surveys have shown that these earthquake swarms are associated with the upwelling of deep-seated fluid. To investigate the nature of the deep-seated fluid, we analyzed 7Li/6Li and 87Sr/86Sr ratios of water samples collected from springs and wells around Ontake volcano in 2000, 2003, 2005, 2007, and 2009. The Li and Sr isotopic compositions of these water samples are largely explained by binary component mixing between near-surface meteoric water and non-surface fluid at each sampling site. On the basis of their Cl/Li and Cl/Sr ratios, we singled out water samples whose Li and Sr isotopic ratios were minimally affected by meteoric water contamination to represent non-surface fluids. The Li and Sr isotopic compositions of most Ontake non-surface fluids, except for samples from the earthquake swarm region, can be explained as the result of volcanic fluids reacting with basement rocks, where they acquired upper crustal signatures. We attribute the fluid associated with the region of earthquake swarms to the lower crust beneath the study area.

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