Abstract
The attenuation of amplitude is seen in seismic waves which pass through the central region of the Aso caldera, in Kyushu, Japan. It is also recognized from spectral analysis of seismic waves that the higher frequencies of the P-wave are reduced in the waves which pass through the central region of the caldera. It is shown that the relative attenuation increases remarkably for the frequency range of 5 to 10 Hz. The specific attenuation factor Q of the P-wave train is about 100. From the surface projection of the ray paths with low Q values through the Aso caldera to each station, the attenuating region is located beneath the center of the caldera, extending to the north of the central cones. In conjunction with the low Q value of the P-wave and the decreases of S-wave amplitudes, the relative P-wave residual times have comparatively large values for seismic waves passing through the central region beneath the caldera. In order to attempt to provide additional information on the depth configuration of the attenuating material, the ray paths of P-wave's first arrivals are located in three-dimensional space. It indicates that the low-velocity material is located beneath the center of the caldera at depths of about 6 to 9 km. However, lowvelocity anomalies above the depth of 6 km and below the depth of 15 km were not able to be detected, because most of the available seismic ray paths had crossed the caldera at depths of about 6 to 15 km. Furthermore, the relative residual times have numerous errors resulting from incorrect hypocenter locations, origin times, inhomogeneities in the structure and uncertainty of the velocity structure. At shallow depths in the Aso caldera, refraction or reflection studies are required for an accurate estimate of the structure and more detailed properties of the attenuating material.
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References
Aki K, Christoffersson A, Husebye ES (1976) Three-dimensional seismic structure of the lithosphere under Montana LASA. Bull Seismol Soc Amer 66:501–524
Anderson DL, Ben-Menaham A, Archambeau CB (1965) Attenuation of seismic energy in the upper mantle. J Geophys Res 70:1441–1448
Aspinall WP, Michael MO, Tomblin J (1976) Evidence for fluid bodies beneath the Sulphur Spring geothermal region, St. Lucia, West Indies. Geophys Res Lett 3:87–90
Balesta ST, Farberov AI, Smirnov VS, Tarakanovsky AA, Zibin MI (1977) Deep crustal structure of the Kamchatkan volcanic regions. Bull Volcanol 40:260–266
Båth M (1974) Spectral analysis in geophysics. (Developments in Solid Earth Geophysics 7) Elsevier, Amsterdam, pp 1–563
Birch F (1958) Interpretation of the seismic structure of the crust in the light of experimental studies of wave velocities in rock. Contr Geophys in Honor B Gutenberg, Pergamon, New York:158–170
Crosson RS, Koyanagi RY (1979) Seismic velocity structure below the Island of Hawaii from local earthquake data. J Geophys Res 84:2331–2342
Eaton GP, christiansen RL, Iyer HM, Pitt AM, Mabey DR, Blank Jr HR, Zietz I, Gettings ME (1975) Magma beneath Yellowstone National Park — new geological and geophysical data indicate the presence of a batholith, in part still molten. Science 188:787–796
Einarsson P (1978) S-wave shadows in the Krafla Caldera in NE-Iceland, evidence for a magma chamber in the crust. Bull Volcanol 41:187–195
Ellsworth WL, Koyanagi RY (1977) Three-dimensional crust and mantle structure of Kilauea Volcano, Hawaii. J Geophys Res 82:5379–5394
Fedotov SA (1968) On deep structure, properties of the upper mantle and volcanism of the Kuril-Kamchatka island are according to seismic data. Geophys Monograph 12:131–139
Fedotov SA, Tokarev PI (1974) Earthquakes, characteristics of the upper mantle under Kamchatka, and their connection with volcanism. Bull Volcanol 37:245–257
Gorshkov GS (1958) On some theoretical problems of volcanology. Bull Volcanol 19:103–114
Gupta HK, Ward RW, Lin TL (1982) Seismic wave velocity investigation at the Geysers-Clear lake geothermal field, California. Geophys 47:819–824
Hirata T, Uchiyama T (1981) Damping area in the Aira Caldera of south Kyushu. Zishin (J Seismol Soc Japan) 34:435–437 (in Japanese)
Ho-Liu P, Kanamori H, Clayton R (1988) Applications of attenuation tomography to Imperial Valley and Coso-Indian Wells regions, southern California. J Geophys Res 93:10501–10520
Iyer HM, Healy JH (1972) Teleseismic residuals at the Lasa-USGS extended array and their interpretation in terms of crust and upper mantle structure. J Geophys Res 77:1503–1527
Iyer HM (1975) Anomalous delays of teleseismic P waves in Yellowstone National Park. Nature 253:425–427
Iyer HM, Evans JR, Zandt G, Stewart RM, Coakley JM, Roloff JN (1981) A deep low velocity body under the Yellowstone caldera, Wyoming, delineation using teleseimic P-wave residuals and tectonic interpretation. Geol Soc Amer Bull 92, part 2:1471–1646
Jackson DD, Anderson DL (1970) Physical mechanisms of seismic-wave attenuation. Rev Geophys Space Phys 8:1–63
Kane MF, Mabey DR, Brace RL (1976) A gravity and magnetic investigation of the Long Valley caldera, Mono Country, California. J Geophys Res 81:754–762
Knopoff L (1964) Q. Revies Geophys 2:625–660
Kubota S, Berg E (1967) Evidence for magma in the Katmai volcanic range. Bull Volcanol 31:175–214
Kubotera A, Tajima H, Sumitomo N, Doi H, Izutuya S (1969) Gravity surveys on Aso and Kuju volcanic region, Kyushu district, Japan. Bull Earthq Res Inst Univ Tokyo 47:215–255
Latter JH (1981) Location of zones of anomalously high S-wave attenuation in the upper crust near Ruapehu and Ngauruhoe volcanoes, New Zealand. J Volcanol Geotherm Res 10:125–156
Long RE, Mitchell MG (1970) Teleseismic P-wave delay time in Iceland. Royal Astr Soc Geophys J 20:41–48
Luetgert JH, Mooney WD (1985) Earthquake profiles from the Mammoth Lake, California, earthquake swarm, January 1983: implications for deep crustal structure. Bull Seismol Soc Amer 75:211–221
Matsumoto T (1971) Seismic body waves observed in the vicinity of Mount Katomai, Alaska, and evidence for the existence of molten chambers. Geol Soc Amer Bull 82:2905–2920
Moriya T, Okada H (1980) Observation of a quarry blast in and around Usu Volcano, travel time and propagation anomaly caused by magma. Kazan (J Volcanol Soc Japan) 25:63–74 (in Japanese)
Murase T, McBirney AR (1973) Properties of some common igneous rocks and their melts at high temperatures. Geol Soc Amer Bull 84:3563–3592
Okubo Y, Graf RJ, Hansen RO, Ogawa K, Tsu H (1985) Curie point depths of the island of Kyushu and surrounding areas, Japan. Geophys 53:481–494
Ono K, Ito K, Hasegawa I, Ichikawa K, Iizuka S, Kakuta T, Suzuki H (1978) Explosion seismic studies in south Kyushu, especially around the Sakurajima Volcano. J Phys Earth 26, Suppl:309–319
Oppenheimer DH, Herkenhoff KE (1981) Velocity-density properties of the lithosphere from three-dimensional modeling at the Geysers-Clear Lake region, California. J Geophys Res 86:6057–6065
Reasenberg PA, Ellsworth W, Watter AW (1980) Teleseismic evidence for a low velocity body under the Coso geothermal area. J Geophys Res 85:2471–2483
Rinehart EJ, Sanford AR (1981) Upper crustal structure of the Rio Grande rift near Socorro, New Mexico, from inversion of microearthquake S-wave reflections. Bull Seismol Soc Amer 71:437–450
Robinson R, Iyer HM (1981) Delineation of a low-velocity body under the Roosevert Hot Springs geothermal area, Utah, using teleseismic P-wave data. Geophys 46:1456–1466
Ryall A, Benett DL (1968) Crustal structure of southern Hawaii related to volcanic process in the upper mantle. J Geophys Res 73:4561–4568
Ryall F, Ryall A (1981) Attenuation of P and S waves in a magma chamber in Long Valley caldera, California. Geophys Res Lett 8:557–560
Sanders CO, Ryall F (1983) Geometry of magma bodies beneath Long Valley, California, determined from anomalous earthquake signals. Geophys Res Lett 10:690–692
Sanders CO (1984) Location and Configuration of magma bodies beneath Long Valley, California, determined from anomalous earthquake signals. J Geophys Res 89:8287–8302
Shimizu H, Mishina M, Ueki S, Hori S, Yamamoto K, Takagi A (1981) Temporalintensive seismological observation at Azuma Volcano. Report Joint Geophys Geochem observations Azuma Volcano:19–40 (in Japanese)
Smith RB, Shuey RT, Pelton JR, Bailey JP (1977) Yellowstone hot spot: contemporary tectonic and crustal properties from earthquake and aeromagnetic data. J Geophys Res 82:3665–3676
Solomon SC (1973) Shear wave attenuation and melting beneath the mid-Atlantic ridge. J Geophys Res 78:6044–6059
Spetzler H, Anderson DL (1968) The effect of temperature and partial melting on velocity and attenuation in a simple binary system. J Geophys Res 73:6051–6060
Stauber DA (1982) Two-dimensional wave velocity structure under San Francisco volcanic field, Arizona, from teleseismic P residual measurements. J Geophys Res 87:5451–5459
Steeple DW, Iyer HM (1976) Low-velocity zone under Long Valley as determined from teleseismic events. J Geophys Res 81:849–860
Sudo Y (1981) Seismic activities at the western region of the Aso caldera. Kazan (J Volcanol Soc Japan) 23:263–279 (in Japanese)
Sudo Y, Yamada T, Masuda H (1984) Seismic activity and focal mechanism around the Aso caldera. Ann Disas Prev Res Inst Kyoto Univ 27B-1:35–44 (in Japanese)
Sudo Y (1988) Upper crustal structure of the Aso caldera. Kazan (J Volcanol Soc Japan) 33:130–134 (in Japanese)
Tokarev PI, Shirokov BA, Zobin BM (1974) Seismicity in the region of the northern group at the Kamchatka volcanoes. Seismicity and Seismic forecasting property in the upper mantle and its relation with volcanism in Kamchatka Nauka:46–52 (in Russian)
Utsu T (1975) Detection of a domain of decreased P-velocity prior to an earthquake. Zishin (J Seismol Soc Japan) 28:435–448 (in Japanese)
Ward RW, Young CY (1980) Mapping seismic attenuation within geothermal systems using teleseisms with application to the Geysers-Clear Lake region. J Geophys Res 85:5227–5236
Ward RM, Schlue JW, Sanford AR (1981) Three-dimensional velocity anomalies in the upper crust near Socorro, New Mexico. Geophys Res Lett 8:553–556
Young CY, Ward RW (1980) Three-dimensional Q -1 model of the Coso Hot springs known geothermal resource area. J Geophys Res 85:2459–2470
Zlobin TK, Popov AA, Fedorchenko VI (1981) Structure of the earth's crust in southern Kunashir Island based on convertwave method data. Geotectonics 15:168–175 (English translation)
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Sudo, Y. An attenuating structure beneath the Aso Caldera determined from the propagation of seismic waves. Bull Volcanol 53, 99–111 (1991). https://doi.org/10.1007/BF00265415
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DOI: https://doi.org/10.1007/BF00265415