Identifikasi Deformasi Tektonik Aktif Berdasarkan Ekstraksi Kelurusan Morfologi dan Seismisitas di Sukabumi, Jawa Barat
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Abstract
The epicenter of the earthquake in Sukabumi has formed subsurface deformation which is now also recorded on the surface area. This is manifested through the geomorphology of the scarp and river lineaments. Extraction of lineaments produced by geological deformation can be used to identify its active tectonic deformation. The research objective is to determine the relationship between the active fault structure and the dominant direction of lineaments in the study area. The Edge Enhancing Filtering method is used to interpret lineaments manually and semi-automatically. The lineament geospatial data was extracted using the Sastratenaya formula to determine the chronology of the lineaments formed. The Sastratenaya formula results showed the lineaments recorded by DEM images data processing, the first segment direction is N315°E and the second is N10°E, both are interpreted as the result of fault reactivation. It can be interpreted that the Cimandiri Fault, which is an active fault that has an N88°E/85° rake 33° sinistral oblique-slip fault movement, affects the lineaments direction of two segments in the research area of Sukabumi, West Java.
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References
[1] G. I. Marliyani, J. R. Arrowsmith, dan K. X. Whipple, “Characterization of Slow Slip Rate Faults in Humid Areas: Cimandiri Fault Zone, Indonesia,” J. Geophys. Res. Earth Surf., vol. 121, no. 12, hal. 2287–2308, 2016, doi: 10.1002/2016JF003846.
[2] E. Gunawan dan S. Widiyantoro, “Active Tectonic Deformation in Java, Indonesia Inferred from a GPS-derived Strain Rate,” J. Geodyn., vol. 123, hal. 49–54, 2019, doi: 10.1016/j.jog.2019. 01.004.
[3] F. Febriani, “Seismicity around the Cimandiri fault zone, West Java, Indonesia,” AIP Conf. Proc., vol. 1711, no. February 2016, 2016, doi: 10.1063/1.4941644.
[4] P. Supendi, A. D. Nugraha, N. T. Puspito, S. Widiyantoro, dan D. Daryono, “Identification of Active Faults in West Java, Indonesia, Based on Earthquake Hypocenter Determination, Relocation, and Focal Mechanism Analysis,” Geosci. Lett., vol. 5, no. 1, 2018, doi: 10.1186/s40562-018-0130-y.
[5] O. M. A. Radaideh, B. Grasemann, R. Melichar, dan J. Mosar, “Detection and Analysis of Morphotectonic Features Utilizing Satellite Remote Sensing and GIS: An Example in SW Jordan,” Geomorphology, vol. 275, hal. 58–79, 2016, doi: 10.1016/j.geomorph.2016.09.033.
[6] L. Han, Z. Liu, Y. Ning, dan Z. Zhao, “Extraction and Analysis of Geological Lineaments Combining a DEM and Remote Sensing Images from the Northern Baoji Loess Area,” Adv. Sp. Res., vol. 62, no. 9, hal. 2480–2493, 2018, doi: 10.1016/j.asr.2018.07.030.
[7] F. D. Indrastomo, I. G. Sukadana, dan Suharji, “Identifikasi Pola Struktur Geologi Sebagai Pengontrol Sebaran Mineral Radioaktif Berdasarkan Kelurusan pada Citra Landsat-8 di Mamuju, Sulawesi Barat,” vol. 38, no. 2, hal. 71–80, 2017, doi: 10.17146/eksplorium.2017.38.2. 3874.
[8] M. Nanda, S. Rizal, F. Abdullah, R. Idroes, dan N. Ismail, “Mapping Faults Distribution Based on DEM Data for Regional Spatial Plan Assessment of Sabang Municipality , Indonesia,” Int. J. Geomate, vol. 19, no. 76, hal. 197–204, 2020.
[9] J. C. Escamilla-Casas dan J. E. Schulz, “Tectonic Interpretation of Topographic Lineaments in the Seacoast Region of New Hampshire, U. S. A.,” Geofis. Int., vol. 55, no. 1, hal. 17–37, 2016, doi: 10.22201/igeof.00167169p.2016.55.1.1709.
[10] S. Pribadi, Afnimar, N. T. Puspito, dan G. Ibrahim, “Characteristics of Earthquake-Generated Tsunamis in Indonesia Based on Source Parameter Analysis,” J. Math. Fundam. Sci., vol. 45, no. 2, hal. 189–207, 2013, doi: 10.5614/j.math.fund.sci.2013.45.2.8.
[11] G. Sarp, “Lineament Analysis from Satellite Images, North-West of Ankara,” 2005.
[12] Yuliastuti, H. Susiati, Y. Daud, dan A. S. Sastratenaya, “Identifikasi Sistem Kelurusan Di Tapak Banten Menggunakan Data Citra Satelit SPOT-5,” JPEN, vol. 15, no. 1, hal. 9–16, 2013, doi: 10.17146/jpen.2013.15.1.1613.
[13] R. M. Mahbub dan H. G. Hartono, “Korelasi Sebaran Gempabumi dan Densitas Kelurusan pada Keamanan Calon Tapak PLTN Bojonegara, Banten,” Kurvatek, vol. 4, no. 2, hal. 93–102, 2019, doi: 10.33579/krvtk.v4i2.1583.
[14] R. G. Thannoun, “Automatic Extraction and Geospatial Analysis of Lineaments and their Tectonic Significance in some areas of Northern Iraq using Remote Sensing Techniques and GIS,” Int. J. Enhanc. Res. Sci. Technol. Eng., vol. 2, no. 2, hal. 1–11, 2013, doi: 10.13140/RG.2.2.20851. 99363.
[15] T. G. Sitharam, P. Anbazhagan, dan K. Ganesha Raj, “Use of Remote Sensing and Seismotectonic Parameters for Seismic Hazard Analysis of Bangalore,” Nat. Hazards Earth Syst. Sci., vol. 6, hal. 927–939, 2006, doi: 10.5194/nhess-6-927-2006.
[16] I. Haryanto, J. Hutabarat, A. Sudradjat, N. N. Ilmi, dan E. Sunardi, “Tektonik Sesar Cimandiri, Provinsi Jawa Barat,” Bull. Sci. Contrib., vol. 15, no. 3, hal. 255–274, 2017.
