Analisis Seismisitas dan Energi Gempabumi di Kawasan Jalur Sesar Opak Oyo Yogyakarta

Nugroho Budi Wibowo, Juwita Nur Sembri

Abstract

The earthquake that occurred in the Region of Yogyakarta caused by fault activity on the surface, such as Opak-Oyo Fault, Dengkeng Fault, Menoreh Fault  and plate tectonic activity in South of Java. Opak-Oyo fault activity reflected from epicenter distribution and earthquake energy. This research aims to analyze the earthquake energy which has epicenter around the Opak-Oyo Fault in spatial and temporal. Based on earthquake catalog from 2008 – 2016, there were 66 earthquake with 11 significant event. Epicenter distribution reflected in seismicity map and for the tectonic parameter use least square method. Seismicity map of Opak Oyo Fault area show that distribution of epicenter in the East and Southeast of fault line with the calculation result of b value by least square method is 0.4. In temporal, there is an increasing trend of events in 2008-2015 and decline trend of earthquake in 2015- 2017. Earthquake energy that released in Opak Oyo Fault area has varies value about 1x105.2 – 1x1012joules. Meanwhile, the energy that associated with the existence of Opak Fault Lines has value between 1x105.2 – 1x109.6 Joule with 10-20 km of hypocenter.The distribution energy has similar pattern with geological formations in that area.

 


Keywords

Opak Oyo Fault, epicenter, seismicity, least square, energy.

Full Text:

PDF

References

Abidin, Z. H., Andreas, H., Meliano, I., Gamal, M., Kusuma, MA., Kimata, F., Ando, M.

Deformasi Koseismik dan Pascaseismik Gempa Yogyakarta 2006 dari Hasil Survei

GPS. Jurnal Geologi Indonesia, Vol.4, No.4, Hal 275.

Bormann, Peter. 2002. Manual Baru: Praktik Stasiun Pengamatan Seismologi (MBPS²).

Jilid 1A. Diterjemahkan oleh: Ibnu Purwana. Jakarta: P.D. Hobie Karya.

Chen, Fei-Poi., Newman, V, Andrew., Wu, Ren-Tso., dan Lin, Ching-Ching.

Earthquake Probabilities and Energy Characteristics of Seismicity Offshore Southwest

Taiwan. Terr Atmos Ocean Sci., Vol 19,No, 6, Hal 697.

Kusky, Timothy. 2008. Earthquakes: Plate Tectonics and Earthquake Hazards. New York:

Infobase Publishing.

Gutenberg, B. dan Richter, F C. 1942.Earthquake Magnitude, Intensity, Energy, and

Acceleration. Bulletin of The Seismological Society of America. Hal. 105.

Analisis Seismisitas dan .... halaman 90

Motamed, R., Ghalandarzadeh, A., Tawhata, I. dan Tabatabei, S.H. 2007. Seismic Microzonation and Damage Assessment of Bam City. Southern Iran: Journal of Earthquake Engineering. Vol 11, No1, Hal 110.

Rohadi, S., Hendra G., Mezak A.Ratag. 2007. Studi Variasi Spatial Seismisitas Zona Subduksi. Jakarta: Program Magister Sains Kebumian, Institut Teknologi Bandung.

Surono, B,Toha,I., Sudarno. 1992. Peta Geologi Lembar Surakarta - Giritontro. Pusat Penelitian dan Pengembangan Geologi, Direktorat Geologi, Departemen Pertambangan Republik Indonesia.

Utsu, T., 1965, A method for determining the value of b in a formula log N = a –

bM showing the magnitude frequency for earthquakes, Geophys. Bull. HokkaidoUniv., 13, 99–103.

Walter, TR., Wang, R., Leuher, BG., Wassermann, J., Behr, Y., Parolais., Anggaini, A., Gunther, E., Sobieseak, M., Grosser, H., Wetzel, H U., Mikereit, C PJ., Sri Broto, Puspito., K, Harjadi P., and Zcshau, J. 2008, The 26 May magnitude 6,4 Yogyakarta Earthquake south of merapi Vulvano : did lahar deposit amplify ground shaking and thus lead to the disaster?. AGU and The Geochecimal Society.Vol 9, No 5.

Refbacks

  • There are currently no refbacks.