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1 1994
2 , 1971,, 1975,, 1988 (2002) Nishimura et al. (2005) Duputel et al. (2009) Piton de la Fournaise Matsushima et al. (2004) (, 2008) 1993 (, 2008) (2009)(2009)(2010) (2010), (2010) (2010) 4km (Fig. 1)(2010) Fig. 1 Multi-folded reflection profiles beneath both the lines NS and EW with conventional reflection analysis. After Yagi (2010). Fig. 2 Velocity structure model around the reflection lines with forward modeling from the first arrivals. After Tsushima (2010). Fig. 3 Shallow reflection structure beneath the line NS with Pseudo-Reflection Profiling. After Imai (2010). (Fig. 2)(2010) 1km (Fig. 3)
3 Fig. 4 The 2009 seismic lines. Topography is described by the contour of a 200-m interstice. Asterisks and the block marks show shot points, and black dots show temporal stations. The symbols A L, A G, and A show the pressure sources after Hidayati et al. (2007). The dashed lines and the thick gray lines which were drawn from these sources show the magma supply way expected. KD:Kita-dake and MD:Minami-dake shot point Table 1. Shot-point location and the shot times. Altitude denotes the height of a charge head. Latitude (WGS84) Longitude (WGS84) Altitude Deg Min Sec Deg Min Sec (m) Shot time Difference from 2008's shot Northin g Easting (m) 09S /12/10 02:27: S /12/10 01:07: S S /12/10 02:17: S /12/10 01:17: S S /12/10 00:17: S /12/10 02:12: S /12/10 01:12: S /12/10 00:07: S S /12/10 01:27: S /12/10 00:27: S S /12/10 02:07: S /12/10 00:12: S S /12/10 00:22: S S /12/10 01:22: S /12/10 02:22: S shot t
4 Fig. 5 The 2009 shot shot records along the line NS. (a) 09S02, (b)09s04, (c)09s12, and (d)09s08. The left end of each plot is for the north end. The location of a shot point is shown 0 km. Each waveform has been normalized at each maximum value. Black circle shows the part which a change can be seen as compared with, (2009
5 Fig. 6 The 2008 shot records along the line NS. (a)08s09, (b)08s10, (c)08s11, (d) 08S12. Plot style is the same as that of Fig. 5. After Iguchi et al. (2009) ,
6 20092 Hidayati et al. (2007) Line NS Line EW , LS8200SD (, 2006) 4.5Hz 24bit 2ms : :00 GPS( SR530) GPS Fig. 4 Appendix 1 X001AX125AX192A Line NSX001BX094BX101B Line EWKAR KAR3KAR (, 2009 GPS2008 Appendix m 20m N ) NS2) 3) Line EW1) C001C0172) B099B102, B ) D001D010 1), 3) ) Line EW 09S m 20kg 1 (Sxx) 09Sxx Sxx(2009) S0109S15 7(09S02, 09S04, 09S08, 09S10, 09S12, 09S13, 09S15) (2009) 09S02:08S09, 09S04:08S10, 09S08:08S12, 09S10:08S06, 09S12:08S11, 09S13:08S13, 09S15:08S m 2008 Table 1. Line NS Fig Fig. 6 Fig. 5(a) (d) Fig. 6(a) (d) Fig. 5(a) 09S02 09S km0.59km/s, 0.041km1.95km/s 09S020.29km0.91km/s, 0.29km 4.42km1.89km/s 09S02 09S020.77km 0.62km/s 09S02, 1981 (2010) (Fig. 3) 09S02(08S09) km/s
7 Fig. 7 The 2009 shot records along the line EW. (a) 09S10, (b)09s12, (c)09s13, (d)09s15. The left end of each plot is the west end. The location of a shot point is shown 0 km. Each trace has been normalized at each maximum value. The black circle shows the part which a change can be seen as compared with the last observation. Fig. 5(b) 09S0409S04
8 0.29km1.44km/s 0.29km1.7km1.74km/s 09S km0.85km/s, 1.76km2.14km/s 1.76km km3.4km/s3.0km2.70km/s Fig. 8 The 2008 shot record of the linr EW. (a) 08S06, (b)08s11, (c)08s13, (d)08s15 The display style of a plot is the same as that of Fig. 7. After Iguchi et al.(2009).
9 Fig. 9 Peak-amplitude distributions in the line NS. (a) 09S02 and 08S09, (b)09s04 and 08S10, (c)09s12 and 08S11, (d)09s08 and 08S12. A vertical axis shows the logarithm of a peak amplitude and a transverse shows hypocentral distance. Cross symbols are 2008's amplitudes and solid diamonds are 2009's amplitudes. Fig. 10 Peak-amplitude distribution in the line EW. (a)09s13 and 08S13, (b)09s15 and 08S15, (c) 09S10 and 08S06. The style is the same as Fig. 9. (1981)09S km/s 2.14km/s 0.85km/s
10 Fig. 11 Examples of traces and their instantaneous rms amplitude (gate width: 0.2 s). The markers point remarkable waveform changes are observed against the previous observation. Amplitude of the waveforms have been normalized for its maximum amplitude. (a) Records at the stations X081A, X082A for the shots 09S04 and 08S10. (b) Instantaneous rms amplitude distribution of (a). (c) Records at the stations X042A, and X043A for the shots 09S12 and 08S11. (d) Instantaneous rms amplitude. A logarithmic vertical axis is applied only in this plot. (e) Records at the stations X092B, X093B, and X094B for the shots 09S13 and 08S13. (f) Instantaneous rms amplitude of X093B. Fig. 5(c) 09S12Line NS 09S120.33km 1.12km/s1.36km4.46km/s 1.36km km 1.94km/s 09S120.47km1.37km/s 8km4.43km/s 09S12(1981) km/s km/s Fig. 5(d) 09S08 09S081.9km3.02km 0.13km0.61km/s 0.13km1.81km3.01km/s 1.9km 1.92km3.02km2.24km 3.02km km1.90km/s 4.72km 09S km0.62km/s0.42km 5.78km/s1.19km2.54km/s 09S08(1981) (2010) 09S08 09S km/s S km 2.24km/s(K7) 09S , 5.58km/s 2009 Line NS 2009 Fig. 6
11 2008 Line EWFig Fig. 8 Fig. 7Fig. 8 Fig. 7(a) 09S10 09S km3.0km/s 1.31km1.49km/s 2.0km9.93km/s 2.92km2.61km/s, 4.57km1.4km/s, 4.95km/s 09S10(1981) S63.0km/s, 1.49km/s 09S122.64km/s Fig. 7(b) 09S12Line EW 09S120.19km 1.12km/s2.89km/s 09S121.51km 1.81km/s3.07km2.35km/s 3.94km4.41km/s (1981) 09S121.12km/s 2.89km/s 09S121.81km/s2.35km/s K6 Fig. 7(c) 09S1309S km2.3km4.07km/s 2.3km2.6km 2.65km2.02km/s 09S km 1.26km/s0.44km1.14km/s 1.55km2.27km/s, 3.39km/s 09S13(1981)K6 09S km/sK6 09S km/s Fig. 7(d) 09S15 09S km0.74km/s Fig. 12 Estimated position of the reflecting points that remarkable changes appeared. The plot style is the same as that in Fig.4. An orange arrow points to the occurence zone of the remarkable enhancement in lataer phases around 3s. Fig. 13 Processing flow and parameter of the single-folded profiling 4.43km2.54km/s 09S150.03km 0.29km/s0.22km 1.06km/s09S15 K4 K4 09S km/sK4 2009
12 Line EW Fig Fig. 9, (08S09, 08S10, 08S11, 08S12, 08S13, 08S15) (Fig. 9(a)(d), Fig. 10(a)(b)) S S (Fig. 10(c)) Fig. 5 Fig. 6 Fig. 5(b) Fig. 5(c) Fig. 5(b) 2008 Fig. 6(b) 3 Fig. 5(c) 2008 Fig. 6(c) Line EW Fig. 7(c) Fig. 8(c) Fig S Fig. 12 Line NSLine EW Line NS09S12 X042A, X043A (Fig. 11(c))Line EW 09S13X092B, X093B, X094B (Fig. 11(e)) Fig. 11(c) (f)fig. 11(a) (2010) Fig Fig. 13 (SFP) Fig. 14 Fig. 14X001A (km)(162m) Fig. 14(a) 2009 Fig. 14(b) 2008 Fig. 14(a) (b) Fig. 14 (a) km1.8(A) 1.2km1.7(B)3.0km3(C) Fig. 14(a) DE 24kmFig. 14(b) 45 Fig. 14(a) CC Fig. 11(a) 3 NMO 3kmB, C A Fig. 14(A) D, EFig. 5
13 Fig. 14 The single-folded profiles (SFP) of the line NS. (a) SFP by the 2009 data. The circles A-E show the part where the remarkable change is observed. (b) SFP based on 2008 data. The cross section projected on the line which connects the stations X125A to X001A. The origin of a distance is the station X001A. A vertical axis is the normal two-way travel time from the datum. The datum is defined at 162 m in height. 析を待って議論を進めたい 準となる2008年観測の測線北端における記録 (Fig. また Hidayati et al. (2007) のモデルからは往復走 6(a)) において相当する走時のS/N比が高くないこと 時5秒以上 6km以上の深さに相当 における構造変 から 現時点では反射波強度の変化の評価は難しい 化が桜島北東部で期待される しかしこの議論の基 と考える 2009年観測を新たな基準として今後得ら
14 G (2009): 2008, 52B, pp (2008):, 10, pp (2010): 21, 102pp. (2002): 1998, 55, pp (2010): (22 3), 11pp. (2006):, 59, pp (2009): 2009 V (1971): 4, Vol. 6, pp (1975):, Vol. 16, pp (1988):, Vol. 40, pp (2010): 21, 111pp. (2009): 2009 B03. (1981):,, 8pp. (2010): 21, 104pp. Duputel, Z., Ferrazzini, V., Brengier, F., Shapiro, N., Campillo, M., and Nercessian, A. (2009): Real time monitoring of relative velocity changes using ambient seismic noise at the Piton de la Fournaise volcano (La Reunion) from January 2006 to June 2007, Journal of Volcanology and Geothermal Research, Vol. 184, pp Matsushima, J., Yokota, T., Okubo, Y., Rokugawa, S., Tanaka, K., Tsuchiya, T., Narita, N., Tani, K. (2004):Repeated seismic reflection measurements in the Kakkonda geothermal field, Journal of Volcanology and Geothermal Research, Vol. 129, pp Nishimura, T., Tanaka, S., Yamamoto, S., Sano, T., Sato, M., Nakahara, H., Uchida, N., Hori, S., and Sato, H. (2005): Temporal changes in seismic velocity of the crust around Iwate volcano, Japan, as inferred from analyses of repeated active seismic experiment data
15 from 1998 to 2003, Earth Planets Space, Vol. 57, pp
16 Appendix 1. Station location. Rank shows a reinstallation rank. Refer to the text for the definition of a reinstallation rank. Station Logger Latitude (WGS84) Longitude (WGS84) Altitude Offset to 2008's station Rank Note Deg Min Sec Deg Min Sec (m) Northi Eastin ng (m) g (m) C C C C Noisy C C Bag broken and drowned logger C Bag broken and drowned logger C Bag broken and drowned logger C Bag broken and drowned logger C C Broken bag, TCAL error C C C Noisy C C C K AR K AR K AR Noisy K AR K AR K AR K AR X 001 A Turned logger and sensor, noisy X 002 A Noisy X 003 A Noisy X 004 A X 005 A Noisy X 006 A X 007 A Noisy X 008 A X 009 A X 010 A X 011 A X 012 A Delayed start for 9 s. X 013 A TCAL error, noisy. X 014 A X 015 A Broken bag X 016 A X 017 A X 018 A Noisy X 019 A X 020 A X 192 A X 021 A Broken bag X 022 A X 023 A X 024 A Failed and no data. Quadruplet flashing indicator ramp. X 025 A X 026 A X 027 A Broken bag X 028 A X 029 A Delayed start for 33 s. X 030 A X 031 A Delayed start for 9 s. X 032 A X 033 A Failed and no data. X 034 A X 035 A X 036 A X 037 A X 038 A X 039 A X 040 A X 041 A Delayed start for 6s. X 042 A
17 Station Logger Latitude (WGS84) Longitude (WGS84) Altitude Offset to 2008's station Rank Note Deg Min Sec Deg Min Sec (m) Northi Eastin ng (m) g (m) X 043 A X 044 A X 045 A X 046 A X 047 A X 048 A X 049 A X 050 A X 051 A X 052 A X 053 A X 054 A X 055 A Delayed start for 9s. X 056 A Failed and no data X 057 A Delayed start for 15 s. X 058 A Noisy X 059 A Noisy X 060 A X 061 A X 062 A Noisy X 063 A Delayed start for 24 s. X 064 A X 065 A X 066 A X 067 A X 068 A X 069 A X 070 A TCAL error X 071 A X 072 A X 073 A X 074 A X 075 A X 076 A X 077 A noisy X 078 A X 079 A X 080 A X 081 A X 082 A noisy X 083 A X 084 A X 085 A X 086 A X 087 A X 088 A X 089 A X 090 A X 091 A X 092 A X 093 A Delayed start for 12 s. X 094 A Delayed start for 6 s. X 095 A X 096 A X 097 A Noisy X 098 A noisy X 099 A X 100 A F: broken bag and noisy X 101 A X 102 A F: moved about 10cm away. X 103 A X 104 A TCAL error X 105 A Noisy X 106 A periodic burst noise X 107 A minutes interval noise burst X 108 A X 109 A Noisy X 110 A X 111 A X 112 A
18 Station Logger Latitude (WGS84) Longitude (WGS84) Altitude Offset to 2008's station Rank Note Deg Min Sec Deg Min Sec (m) Northi Eastin ng (m) g (m) X 113 A Noisy X 114 A Noisy X 115 A X 116 A TCAL error X 117 A X 118 A X 119 A X 120 A Noisy X 121 A X 122 A X 123 A Noisy and doubtful location of 2008's station X 124 A Opened bag X 125 A D Noisy D Noisy D D Noisy D D D Noisy D D Noisy D Noisy X 001 B Noisy X 002 B X 003 B X 004 B Drifting base level X 005 B X 006 B Noisy X 007 B Delayed start for 6 s, and noisy. X 008 B X 009 B Bag broken and short receptacle lost X 010 B Broken bag X 011 B Noisy X 012 B Noisy X 013 B X 014 B Noisy X 015 B Absolutely noisy X 016 B Noisy, doubtful location of 2008's description X 017 B Noisy X 018 B Noisy X 019 B Noisy X 020 B X 021 B TCAL error and noisy X 022 B X 023 B X 024 B X 025 B X 026 B X 027 B X 028 B X 029 B X 030 B X 031 B X 032 B Noisy X 033 B X 034 B X 035 B Noisy X 036 B X 037 B TCAL error X 038 B X 039 B Failed and no data X 040 B X 041 B X 042 B X 043 B X 044 B Noisy
19 Station Logger Latitude (WGS84) Longitude (WGS84) Altitude Offset to 2008's station Rank Note Deg Min Sec Deg Min Sec (m) Northi Eastin ng (m) g (m) X 045 B Noisy X 046 B X 047 B X 048 B noisy X 049 B X 050 B X 051 B Noisy B X 101 B B B B Early retrieval Early retrieval, periodic burst noise B Early retrieval, and 4 minutes interval burst noise B Early retrieval, TCAL error, 4 minutes interval burst noise B Early retrieval B Early retrieval, 1 minutes interval burst noise B Early retrieval X 054 B Delayed start for 6 s, noisy X 055 B X 056 B Delayed start for 6 s X 057 B X 058 B X 059 B X 060 B X 061 B X 062 B X 063 B Failed and no data X 064 B X 065 B X 066 B X 067 B X 068 B X 069 B Noisy X 070 B X 071 B X 072 B Noisy X 073 B X 074 B X 075 B X 076 B X 077 B TCAL error X 078 B X 079 B Noisy X 080 B Noisy X 081 B X 082 B Noisy X 083 B Noisy X 084 B noisy X 085 B X 086 B Noisy X 087 B TCAL error and noisy X 088 B Broken bag X 089 B Dewed bag inside X 090 B X 091 B X 092 B X 093 B Broken bag and drawed away. X 094 B
20 The Repeated Seismic Survey 2009 in Sakurajima Volcano, South Kyushu, Japan Tomoki TSUTSUI *, Masata IGUCHI, Takeshi TAMEGURI, Yoshihiro UEDA **, Hiromitsu Oshima ***, Sadato UEKI ****, Takao Ohminato *****, Jun OIKAWA *****, Mie ICHIHARA *****, Kenji NOGAMI ******, Haruhisa NAKAMICHI *******, Takahiro Ohkura ********, Hiroshi SHIMIZU *********, Hiroki MIYAMACHI **********, Hiroshi YAKIWARA **********, Tokumitsu MAEKAWA ***, Shinichiro HORIKAWA *******, Shin YOSHIKAWA ********, Tadaomi SONODA, Shuichiro HIRANO **********, Koichi SUEMINE **, Mikita HAYASHI **, Koji KATO **, Jun NAGAO **, Takamitsu IKEGAME **, Shinichi MATSUSUE **, Hirohito GOTO **, Taisuke KOHNO **, Takahiro YANADA ****, Madoka TANAKA ****, Ryuichi WATANABE *, Yutaka NAGAOKA *****, Yuki MAEHARA ******(currently*****), Sayumi YOSHIDA *******, Yumi KOBAYASHI *******, and Shiro KAYAHASHI ********* *Faculty of Engineering and Resource Science, Akita University, ** Japan Meteorological Agency ***Graduate School of Science, Hokkaido University, **** Graduate School of Science, Tohoku University, ***** Earthquake Research Institute, University of Tokyo, ****** Volcanic Fluid Research Center,Tokyo Institute of Technology, ******* Graduate School of Environmental Studies, Nagoya University, ******** Graduate School of Science, Kyoto University, ********* Faculty of Science, Kyushu University, ********** Faculty of Science, Kagoshima University, Synopsis The repetitive seismic prospecting was performed in Sakurajima Volcano on December 2009, aiming at a detection of the structural change accompanying volcanic activity. Sakurajima Volcano is a favorable field to examine a monitoring method because of its enhancing activity and abundant background information. A part of the seismic lines of the 2008's survey was reconstructed and was performed the seismic exploration against transition of such volcanic activity. The seismic lines consisted of 15 shot points, and 263 temporal seismic stations. Among these, the reconstructed line consisted of seven reappearance shot-points, and 219 reappearance temporal stations. In reconstruction of a line, 202 points succeeded in the re-installation to the original point. As compared with the previous observation with the same charge size, 0.6 to 2.9 times of the peak amplitude was obtained by the shots. Although no change in the first-arrival time was conspicuous is observed in the obtained record, a systematic change is observed in later phases of the observation record in a northeast part of the covered area. Therefore, it is expected that obtained data may leads to a detection of the structural change accompanying activity of the Sakurajima volcano. Keywords: Sakurajima Volcano, Artificial explosion experiment, Structure transition monitoring
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