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"Gempa Bumi Besar Jepang Timur atau Higashi Nihon Daishinsai yang terjadi pada tahun 2011 memberikan dampak negatif terhadap perekonomian Jepang secara luas. Dalam situasi krisis tersebut, pemerintah Jepang mengkaji The New Growth Strategy 2010 untuk mengatasi perekonomian negara. Tertulis dalam The New Growth Strategy 2010 bahwa pariwisata merupakan salah satu pilar industri yang dapat memperbaiki perekonomian Jepang. Pemerintah membuat perencanaan pariwisata yang disebut Tourism Nation Promotion Basic Plan 2012 untuk mengembangkan pariwisata Jepang. Selama pelaksanaan, berbagai upaya yang dilakukan pemerintah Jepang telah menunjukan perkembangan pariwisata yaitu dengan tercapainya beberapa target perencanaan sehingga pertumbuhan ekonomi Jepang dalam bidang pariwisata meningkat

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The Great East Japan Earthquake or Higashi Nihon Daishinsai which occurred by 2011 had a negative impact to Japanese economy at large. On that crisis situation, the Japanese Government reviewed The New Growth Strategy 2010 to tackle country?s economy. The New Growth Strategy 2010 says that tourism is one of the pillar which can improve Japanese economy. Then, the Government made Tourism Nation Promotion Basic Plan 2012 to develop tourism in Japan. During implementation, various efforts has shown the development of tourism achieved some targets so the economic growth of Japan in the field of tourism has increased."

"Makalah ini memaparkan hasil pengembangan beberapa model acuan untuk menentukan jumlah stasiun pencatat percepatan gempabumi kuat pada tingkatan negara berdasarkan kondisi geografis, demografis, dan sosial-ekonomi. Beberapa model ini dapat digunakan dalam pengembangan lebih lanjut sistem pencatat gempa bumi kuat Indonesia. Dasar pengembangan model adalah sistem serupa di Selandia Baru, Jepang, Taiwan, Iran, Turki, dan Italia. Parameter jumlahstasiun pencatat yang diusulkan adalah jumlah stasiun per 1000 km2luas daratan, dan tiga buah model regresi eksponensial telah dikembangkan berdasarkan fungsi kepadatan penduduk negara, fungsiProduk Domestik Bruto (PDB) per kapita, dan fungsi Indeks Daya-Saing Global (GCI) kelompok Persyaratan Dasar. Berdasarkan tiga modelini, jumlah minimum stasiun pencatat yang dibutuhkan adalah sekitar 750 stasiun.

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AbstractAn empirical study to develop benchmark models at country-level to assess the suggested number of earthquake strong-motion stations based on a framework encompassing geographic, demographic, and socio-economic parameters is reported. The models are to provide a working estimate of the required number of stations for improving the strong-motion instrumentation program of Indonesia. National earthquake strong-motion networks of New Zealand, Japan,Taiwan, Iran, Turkey, and Italy were used as the references.The parameter proposed is the number of stations in land area of 1,000 km2, and three models based on the exponential regression analysis are presented as functions of population density, Gross Domestic Product (GDP) per capita, and the Global Competitiveness Index (GCI) Basic Requirements Index. Using the models, it is suggested that Indonesia would require at least 750 stations."

"To identify factors affecting satisfaction with service recovery of banking sector and overall satisfaction, together with the effect of customersatisfaction on repurchase intent and word-of-mouth intent in the banking in Vietnam, a survey is conducted on 215 customers.Those respondents, who are buying services from the bank, namely Vietnamese Local Bank (VLB), have experienced in service failure and service recovery in their transaction with VLB, and lived in Ho Chi Minh City. Structural equation model (SEM) is employed to estimate the theoretical model and to test hypotheses. The findings of the study showed that distributive justice positively impact customer satisfaction with service recovery, and overall satisfaction. Satisfaction with recovery has a strong impact on overall satisfaction. Both satisfaction with recovery and overall satisfaction disclose a positive influence on repurchase intent, and only satisfaction with recovery positively affecting word-of-mouth intent."

"Tinjauan karakteristik zona seismogenik terkait dengan proses rupture gempabumi di zona Subduksi Sumatera telah dilakukan dengan berbagai metode. Zona ini tercatat pernah mengalami beberapa gempa besar yaitu gempabumi Aceh 2004 Mw=9,1, Nias-Simeulue 2005 Mw=8,6, Bengkulu 2007 Mw=8,5, dan Enggano 2000 Mw=7,9. Penelitian ini memfokuskan hubungan antara analisis kontras densitas berdasarkan data gravitasi satelit GOCE dengan distribusi slip di zona rupture empat gempabumi besar yang pernah terjadi. Pemrosesan data gravitasi satelit dilakukan untuk mendapatkan data Gravity disturbance (Gd) dan turunan vertikal gravitasi (Tzz) yang dikoreksi oleh efek topografi dan sedimen dengan dekomposisi spektrum yang berbeda-beda untuk mendapatkan peta gravitasi dengan kedalaman yang berbeda-beda. Berdasarkan analisis Tzz, slip maksimal rupture gempabumi berkorelasi dengan pola Tzz minimal dan kontras densitas rendah, sementara itu rupture berakhir pada pola Tzz maksimal dan kontras densitas tinggi. Pola Tzz dan Gravity disturbance dapat menggambarkan posisi barrier dan asperitas dari zona subduksi Sumatra. Peta skematik berhasil menggambarkan segmentasi seismik Subduksi Sumatra yang memiliki zona asperitas sepanjang strike subduksi yang berhubungan dengan Tzz minimal dan berhubungan dengan zona forearc, serta adanya barrier yang berhubungan dengan Tzz maksimal yang merupakan manifestasi dari struktur (fracture zone dan seamount) yang tersubduksi ke lempeng samudra.

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The review of the characteristics of the seismogenic zone associated with the earthquake rupture process in the Sumatra Subduction Zone has been carried out by various methods. This zone has experienced several major earthquakes, namely the Aceh 2004 Mw=9,1, Nias-Simeulue 2005 Mw=8,6, Bengkulu 2007 Mw=8,5, and Enggano 2000 Mw=7,9. This study focuses on the relationship between density contrast analysis based on gravity data from the GOCE satellite and the slip distribution in the rupture zones of four major earthquakes that have occurred. Satellite gravity data processing was carried out to obtain data for Gravity disturbance (Gd) and vertical gravity derivatives (Tzz), which are corrected by topography and sediment effects with different spectrum decomposition to get gravity maps with different depths. Based on the Tzz analysis, the maximal slip of the earthquake rupture is correlated with the minimal Tzz pattern and low-density contrast. In contrast, the rupture ends at the maximum Tzz pattern and high-density contrast. Tzz pattern and Gravity disturbance can describe the barrier position and asperity of Sumatra subduction zone. The schematic map succeeds in portraying the seismic segmentation of Sumatra Subduction which have asperities zone along the subduction strike associated with the minimal Tzz and associated with the forearc zone, as well as the barrier related to the maximum Tzz which is a manifestation of structures (fracture zone and seamount) that are subducted to the oceanic plate."

"Gempabumi yang terjadi di Yogyakarta 27 Mei 2006 merupakan gempabumi besar dengan kekuatan Mw : 6, 2. Selain menyebabkan kematian sekitar 5000-an jiwa, juga mneyebabkan kerusakan infrastruktur serta mengakibatkan kerusakan geologi berupa hilangnya kekuatan tanah atau likuifaksi. Penelitian ini ingin mengungkapkan kaitan kejadian likuifaksi dengan geologi dan indeks keburukan likuifaksi serta pola wilayah bahaya likuifaksi di Daerah Istimewa Yogyakarta menggunakan metode deskriptif dengan pendekatan spasial (keruangan). Hasil penelitian menunjukkan sebaran titik kejadian likuifaksi cenderung mengelompok di tengah wilayah penelitian, sebarannya mengikuti : sebaran jenis batuan endapan Gunungapi Merapi muda, sebaran umur batuan kuarter. Seluruh titik kejadian likuifaksi dijumpai pada jarak kurang dari enam kilometer dari sesar utama dan sesar minor. Sebaran kejadian likuifaksi tidak selalu dijumpai pada wilayah dengan nilai LSI yang besar. Wilayah bahaya likuifaksi terbagi menjadi : wilayah bahaya likuifaksi sangat tidak aman, tidak aman, dan wilayah aman.

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The Yogyakarta earthquake of May 27, 2006 has magnitude Mw : 6,2. This earthquake caused about 5000 died people and destroyed infrastructures also liquefaction. Focus of this study is interrelation between liquefaction occurance and geological condition and liquefaction severity index (LSI). This research is descriptive and spatial approach. The research shows that distribution of liquefaction occurrence is clustered in the centre part of Yogyakarta Special Province, it is related to young volcanic deposits of Merapi Volcano distribution and Quarternary deposits distribution. Liquefaction occurance is situated within 6 km distance from the major and minor fault zone.The distribution of liquefaction occurance it isn?t related to liquefaction severity index (LSI)."

"In this research the model of earth layers between earthquake's epicenter in Hokkaido Japan and observation station in Black Forest of Observatory (BFO), Germany is investigated. The earth model is 1-D that represents the average speed model. The earth model is obtained by seismogram comparison between data and synthetic seismogram in time domain and three components simultaneously. Synthetic Seismogram is calculated with the Green's function of the Earth by MINor Integration (GEMINI) program, where program's input is initially the earth model IASPEI91, PREMAN and also the Centroid Moment Tensor (CMT) solution of the earthquake. A Butterworth low-pass filter with corner frequency of 20 mHz is imposed to measured and synthetic seismogram. On seismogram comparison we can find unsystematic discrepancies, covering the travel time and waveform of all wave phases, namely on P, S, SS wave and surface wave of Rayleigh and Love. Solution to the above mentioned discrepancies needs correction to the earth structure, that covering the change of earth crust thickness, the gradient of �?�h and value of zero order coefficient in �?�h and �?�v in upper mantle, to get the fitting on the surface wave of Love and Rayleigh. Further correction to accomplish the discrepancies on body waves is conducted on layers beneath upper mantle down to depth of 630 km, where a little change at speed model of P and S wave is carried out. The number of oscillation amount especially on Love wave is influenced by earth crust depth earth. Good fitting is obtained at phase and amplitude of Love wave, but also at amplitude of some body wave too. This effect is not yet been exploited for the determination of moment tensor."