Pulinets, S.A. and Dunajecka, M.A., 2007, Specific variations of air temperature and relative humidity around the time of Michoacan earthquake MB.1 Sept. 19, 1985 as a possible indicator of interaction between tectonic plates, Tectonophysics 431 (2007) 221-230. Saroso, S., Ishikawa, H., Hattori, K., Hayakawa, M., Liu, J.Y., Shiokawa, K., and Yumoto, K., 2006, Uif Geomagnetic Anomaly Related With The Sumatra Earthquakes, Proceedings of the International Workshop on Integration of Geophysical Parameter as a Set of Large Earthquake Precursors, Research and Development Center BMG, Jakarta. Scholz, C.H., The frequency-magnitude relation of microfracturing in rock and its relation to earthquakes, Bull. Seismol. Soc. Am., 58, 399-415, 1968. Scholz, C.H., Sykes, L.R., Aggarwal, Y.P., 1973. Earthquake prediction: a physical basis. Science 181, 803-809. Schorlemmer, D., S. Wiemer, and M. Wyss (2005L Earthquake statistics at Parkfield, Stationarity of b-values, J. of Geophys. Res . 109, B12307, doi10.1029 /2004 JB003234. Shi, Y., and B.A. Bolt, The standard error of the magnitude-frequency bvalue, Bull. Seismol. Soc. Am., 72, 1677-1687, 1982. Telford, W.M., Geldart, L.P., and Sheriff, R.E., 1990, Applied Geophysics, second edition, Cambridge University Press, London Toutain, J.-P., Baubron, J.-c., 1998. Gas geochemistry and seismotectonics: a review. Tectonophysics 304, 1-27. Tsapanos, T., b-value of two tectonic parts in the circum-Pacific belt, Pageoph, 143, 229-242, 1990. Utsu, T. (1965) A method for determining the value of b in a formula log n =a- bM showing the magnitude- frequency relation for earthquakes, Geophys Bull Hokkaido Univ., 13,99-103 (in Japanese). Utsu, T., A method for determining the value of b in a formula of log N=a-bM showing the magnitude frequency relation for earthquakes, Geophys. Bull. Hokkaido Univ., 13,99-103, 1965. /ntegrasi Pengamatan Parameter Geofisika da/am Usaha Prediktabi/itas Gempabumi 70
Wang, J.H. and Lee, C.W., Multifractal measures of earthquakes in west Taiwan, Pure appl. Geophys., 146, 131-145, 1996. Wid iya ntoro, S. & Van der Hilst, R.D., 1996, "Structure and evolution of lithospheric slab beneath the 5unda arc, Indonesia", Science, 271,1566-1570. Wiemer 5, 5., and M. Wyss, (2002), Mapping spatial variability of the frequencymagnitude distribution of earthquakes, Adv. Geophys., 45, 259-302. Wiemer 5., and M. Wyss, (2002), Mapping spatial variability of the frequencymagnitude distribution of earthquakes, Adv. Geophys., 45, 259-302. Yumoto, K. and The MAGDA5 Group, 2006, MAGDAS Project and Its Application For Earthquake Prediction, Proceedings of the International Workshop on Integration of Geophysical Parameter as a Set of Large Earthquake Precursors, Research and Development Center BMG, Jakarta. Integrasi Pengamatan Parameter Geofisika da/am Usaha Prediktabi/itas Gempabumi 71
- Page 1 and 2:
LAPORAN AKHIR INTEGRASI PENGAMATAN
- Page 3 and 4:
LEMBAR IDENTITAS DAN PEN GESAHAN J
- Page 5 and 6:
PRAKATA Penelitian tentang "Integr
- Page 7 and 8:
11.5 Prekursor Magnetik dan Elektro
- Page 9 and 10:
DAFTAR GAM BAR Halaman Gambar 2.1.
- Page 11 and 12:
(d) Cut at 2006, 3 (e) . Cut at 200
- Page 13 and 14:
BABI. PENDAHULUAN 1.1. Latar Belak
- Page 15 and 16:
akan saling menguatkan dalam interp
- Page 17 and 18:
BAB II. TINJAUAN PUSTAKA 11.1. Tat
- Page 19 and 20:
1410 km 410 km 660 km Anomali kecep
- Page 21 and 22:
MMI (Modified Mercalli Intensity).
- Page 23 and 24:
dapat diprediksi dengan penerapan h
- Page 25 and 26:
kecepatan relatif gerak lempeng di
- Page 27 and 28:
Bath's (Richter, 1958, hal 69) memb
- Page 29 and 30:
dilakukan berdasarkan pengamatan pr
- Page 31 and 32:
di sekitar retakan (Mizutani et aI.
- Page 33 and 34: ' Q) D E :::J c: Q) > OJ:: o "3 E
- Page 35 and 36: Sehingga Jumlah frekuensi kumulatif
- Page 37 and 38: umi. Dapat dilihat pada ga mbar 2.9
- Page 39 and 40: 2. Stasiu n ya ng memiliki karakter
- Page 41 and 42: edundansi yang ada dalam skema pyra
- Page 43 and 44: operasi filter terse but. Filter lo
- Page 45 and 46: frekwensi}. 256 sampel ini merupaka
- Page 47 and 48: e. Perhitungan nilai-b, nilai-a, pe
- Page 49 and 50: 111.2. Pengolahan dan Analisis Dat
- Page 51 and 52: le bih sedikit diband ingkan pada w
- Page 53 and 54: identifikasi dari NOAA dan ISC. Ada
- Page 55 and 56: sekitar empat hingga lima tahun. Pe
- Page 57 and 58: 2 1.8 1.6 1.4 1.2 Cl) ..2 ns 1 =i"
- Page 59 and 60: 300 200 100 o 104 0 E 30' 10 50E 30
- Page 61 and 62: ~S r-~~ ·~~ r~~-·~~· -~~~,- · -
- Page 63 and 64: :we 17. 150 125 100 75 50 25 o 197$
- Page 65 and 66: Gambar 4.14. Variasi harian data ma
- Page 67 and 68: diduga sebagai prekursor gempabumi.
- Page 69 and 70: Agustus 2010 (G ambar 4.18) menunju
- Page 71 and 72: II , . '.1.: ~ i ; .', l :i~: ~ o j
- Page 73 and 74: untuk beberapa gempa bumi terkini d
- Page 75 and 76: kelembaban relatif. Proses fisis ya
- Page 77 and 78: gempabumi. Demikian juga dengan par
- Page 79 and 80: BAB V. KESIMPULAN DAN SARAN V.l. K
- Page 81 and 82: DAFTAR PUSTAKA Aki, K. 1965, Maksi
- Page 83: Khatri, K. N., Fractal description