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Seismic radiation by magma injection: An anomalous seismic event near Tori Shima, Japan

Kanamori, Hiroo and Ekström, Göran and Dziewonski, Adam and Barker, Jeffrey S. and Sipkin, Stuart A. (1993) Seismic radiation by magma injection: An anomalous seismic event near Tori Shima, Japan. Journal of Geophysical Research. Solid Earth, 98 (B4). pp. 6511-6522. ISSN 2169-9313. https://resolver.caltech.edu/CaltechAUTHORS:20141028-162534284

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Abstract

The earthquake with a bodywave magnitude m_b=5.5, which occurred near Tori Shima, Japan, on June 13, 1984 (origin time: 0229:25.3 UT, 31.448°N, 140.036°E, depth of 10 km, m_b =5.5, M_S=5.5) is anomalous because it generated tsunamis which are disproportionately large for the magnitude of the earthquake. At Hachijo Island, 150 km from the epicenter, tsunamis were visually observed with peak-to-peak amplitude of 130 to 150 cm. Long-period seismic radiation is also anomalous. Love waves are almost absent, and Rayleigh waves are radiated with equal amplitude and phase in all directions. A simple double-couple model cannot explain these observations. With the assumption of no net volume change at the source, these data can be best explained with a compensated linear vector dipole (CLVD) with the principal tensional dipole in the vertical direction. The scalar moment of this dipole is 4×10^(24) dyn cm. Moment tensor inversions of long-period body waves and surface waves yield an almost identical solution. This CLVD source can be interpreted as horizontal fluid injection. The location of the event is in the Smith depression which is one of the nascent back arc basins just behind the Bonin arc. These basins are filled with thick sediments, and numerous young volcanoes are found near this site. Magmatic injection is most likely to occur in this tectonic environment. However, the time scale of the seismic event seems too short for magma injection to occur. A more likely mechanism involves water-magma interaction. The injection may be viewed as hydrofracturing driven by supercritical water heated by injected magma. The estimated volume of injected water is about 0.018 km^3 and that of basaltic magma is about 10% of this. This type of deformation is more efficient for tsunami generation than faulting with the same scalar moment.


Item Type:Article
Related URLs:
URLURL TypeDescription
http://dx.doi.org/10.1029/92JB02867DOIArticle
http://onlinelibrary.wiley.com/doi/10.1029/92JB02867/abstractPublisherArticle
ORCID:
AuthorORCID
Kanamori, Hiroo0000-0001-8219-9428
Additional Information:Copyright 1993 by the American Geophysical Union. (Received April 29, 1992; revised November 19, 1992; accepted December 4, 1992.) Paper number 92JB02867. We benefitted from discussions with many colleagues when the initial draft was written in 1986, to mention a few: Brad Hager, Don Anderson, Ed Stolper, Akira Kubotera, Katsuyuki Abe, Tokutaro Hatori, Barclay Kamb, Tom Heaton, Emile Okal, and Herbert Shaw. Reviews by Tom Heaton and Greg Beroza were helpful in making the final revision. Collaboration with Kenji Satake on interpretation of tsunamis helped us a great deal in finalizing the model. This work was partially supported by NSF grant EAR 89-15987 and U .S. Geological Survey grant 14-08-0001-G1356. Contribution 5142, Division of Geological and Planetary Sciences, California Institute of Technology.
Funders:
Funding AgencyGrant Number
NSFEAR 89-15987
USGS14-08-0001-G1356
Other Numbering System:
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Caltech Division of Geological and Planetary Sciences5142
Issue or Number:B4
Record Number:CaltechAUTHORS:20141028-162534284
Persistent URL:https://resolver.caltech.edu/CaltechAUTHORS:20141028-162534284
Usage Policy:No commercial reproduction, distribution, display or performance rights in this work are provided.
ID Code:50968
Collection:CaltechAUTHORS
Deposited By: George Porter
Deposited On:28 Oct 2014 23:43
Last Modified:09 Mar 2020 13:18

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