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Hypocenter relocation of earthquake swarm around Jailolo volcano, North Molucca, Indonesia using the BMKG network data: Time periods of September 27-October 10, 2017

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AIP Conference Proceedings 2018年第1期1987卷

作者： Andri Dian Nugraha Pepen Supendi Sri Widiyantoro Daryono Samsul Wiyono 1Global Geophysics Research Group Faculty of Mining and Petroleum Engineering Institut Teknologi Bandung Bandung 40132 Indonesia 2Geophysical Engineering Study Program Faculty of Mining and Petroleum Engineering Institut Teknologi Bandung Bandung 40132 Indonesia 3Agency for Meteorology Climatology and Geophysics (BMKG) Bandung Indonesia 4Agency for Meteorology Climatology and Geophysics (BMKG) Jakarta Indonesia

A year after the hundreds of earthquake swarm last year (2015-2016), recent swarm activity in Jailolo, north of Maluku area, Indonesia began to reactivated. We have successfully relocated 108 out of the 130 earthquake swarm from September 27 to October 10, 2017 by using the BMKG network data through hypocenter double-difference method. The results indicate improvement in hypocenter location, where the initial earthquake focal depths fixed at a depth of 10 km has been updated. A validation through the histogram of travel-time residual depicts good relocation results, in which the residual values are mostly close to zero. The relocated hypocenters are located close to Jailolo volcano area which has focus depths of about 5 – 30 km. We analyzed of waveform of several swarm events (with largest and smallest magnitude) which are recorded by the nearest BMKG station and show has frequency range of 2 to 8 Hz. Our preliminary interpretation, these swarm events probably associated with stress change due to combination of tectonic and deep magma activity in the area.

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Preliminary study results of crustal structure beneath Mount Merapi, Central Java, Indonesia

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AIP Conference Proceedings 2018年第1期1987卷

作者： Sandy Kurniawan Suhardja Sri Widiyantoro Mohamad Ramdhan J.-P. Métaxian 1Department of Geophysical Engineering Faculty of Exploration and Production Pertamina University Jakarta 12220 Indonesia 2Global Geophysics Research Group Faculty of Mining and Petroleum Engineering Bandung Institute of Technology Bandung 40132 Indonesia 3Earth Sciences Study Program Faculty of Earth Sciences and Technology Bandung Institute of Technology Bandung 40132 Indonesia 4ISTerre IRD R219 CNRS Université de Savoie Mont Blanc Le Bourget-du-Lac France

In this study, we put an effort to estimate crustal depth and image crustal structure beneath Merapi volcano by employing multicomponent analysis popularly known as Receiver Function technique. We collected a series of waveforms from teleseismic events recorded from October 2013 to mid-April 2015 at 53 stations as a part of DOMERAPI project. We processed selected seismograms by simple deconvolution process between radial and vertical components to estimate the depth of Moho discontinuity beneath the volcano. Current results show complex structure beneath the volcano and a relatively potential Moho depth at about 30 km, which becomes shallower to the North at about 23 km. Stations located at Southern and Northern area show potential low velocity zone though a velocity modelling is necessary to confirm its depth and how low the velocity is.

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Application of tomography seismic for subsurface modeling of Kelud Mountain

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AIP Conference Proceedings 2016年第1期1730卷

作者： R. Destawan A. Bernando M. Aziz I. R. Palupi Geophysical Engineering Study Program Faculty of Mineral Technology UPN “Veteran” Yogyakarta Indonesia

Kelud is a Quaternary volcano formed by the collision between the Indo-Australian plate with the Eurasian plate, exactly in the south of Java. This volcano is included in stratovolcanoes type explosive eruption characteristics. In order observation of subsurface conditions, performed imaging tomography. The research used data recordings from the 4 point observation in 2007. The data processing started from the initial velocity modeling, ray tracing calculations using the method of bending and tomographic velocity model Vp, Vs and Vp/Vs using inversion techniques delay time. Based on the research activities carried out, were resulted velocity structure models Vp, Vs, Vp/Vs and the hypocenter distribution of volcanic earthquakes occurring in Kelud. Velocity structures of Vp and Vs with variations of negative values between -60 to 0% and the value of Vp / Vs positive indicating the presence of hot fluid Kelud from top to sea level. While the positive values of Vs velocity structure between 0 to 20%, which dominate the east and south peaks interpreted as the rest of the frozen magma from previous volcanic activity.

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Preliminary result of 3-D attenuation tomography beneath Sunda Strait and western part of Java

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AIP Conference Proceedings 2017年第1期1857卷

作者： Muhajir Anshori Andri Dian Nugraha Nanang T. Puspito 1Master Student of Earth Science Study Program Faculty of Earth Sciences and Technology InstitutTeknologi Bandung Indonesia 2Indonesian Meteorological Climatological and Geophysical Agency (MCGA) Indonesia 3Global Geophysics Research Group Faculty of Mining and Petroleum Engineering InstitutTeknologi Bandung Indonesia

Sunda strait lies in the transition zone of two different subduction system that is almost perpendicular to the subduction in southern Java and oblique subduction in western Sumatra. The series of major disasters such as earthquakes and volcanic eruptions is a manifestation of its tectonic setting complexity. We used selected waveform data from724 earthquakes that occurred around the Sunda strait and western part of Java from 2009 – 2015 recorded by 21 MCGA network stations to construct three dimensional image of seismic attenuation. Frequency independent attenuation operators (t*) was determined using spectral fitting method for P and S wave arrivals, respectively. The inversion was performed using simul2000 algorithm to image the lateral and vertical variations of Qp and Qs value in the Sunda Strait and western part of Java. Some interesting features such as subducting slab, mantle wedge, magma chamber under volcanos and fault zones can be imaged well.

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3D Geothermal Modelling Using Gravity Survey on Dolok Marawa, Simalungun District, North Sumatera

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IOP Conference Series: Earth and Environmental Science 2016年第1期29卷

作者： A Rivandi R Destawan Z R Fajri W Hidayat Geophysical Engineering Study Program Faculty of Mineral Technology UPN 'Veteran' Yogyakarta Indonesia

In North Sumatera, gravity method is applied to identify the geothermal model. This method measured the earth gravitational field. This research has 160 measurement points covering 9 square kilometers. We obtained complete Bouguer anomaly values ranging 85 mGal - 130.68 mGal interpreted as a heat source of andesitic igneous rocks that are affected by the presence of Mount Bahtopu magma chamber. We interpreted the values between 40 mGal - 80 mGal as reservoir and caprock. The 3D gravity inverse modelling conducted using Gravblox, and identifying the following lithologies; Toba Pyroclastic Fall (Qjt) with density 1.92 g/cm3, Toba Pyroclastic Flow (Qjt) with density 2.00 g/cm3, Mount Bahtopu Andesite (Qlb) with density 2.4 g/cm3, and 2.6 g/cm3 which is interpreted as heat source in form of andesitic rock and Mount Bahtopu magma chamber. This heat source is estimated to be at a depth of 1.45 km to 3.78 km below the surface.

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Mapping of earthquakes vulnerability area in Papua

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AIP Conference Proceedings 2016年第1期1730卷

作者： Muhammad Fawzy Ismullah M. Muh. Altin Massinai 1Master Program Geophysical Engineering Faculty of Mining and Petroleum Engineering (FTTM) Bandung Institute of Technology (ITB) 10 th Ganesha Street Bandung 40116 West Java INDONESIA 2Geophysics Program Study Faculty of Mathematics and Natural Sciences Hasanuddin University (UNHAS) Perintis Kemerdekaan Km. 10 Street Makassar 90245 South Sulawesi INDONESIA

Geohazard is a geological occurrence which may lead to a huge loss for human. A mitigation of these natural disasters is one important thing to be done properly in order to reduce the risks. One of the natural disasters that frequently occurs in the Papua Province is the earthquake. This study applies the principle of Geospatial and its application for mapping the earthquake-prone area in the Papua region. It uses earthquake data, which is recorded for 36 years (1973-2009), fault location map, and ground acceleration map of the area. The earthquakes and fault map are rearranged into an earthquake density map, as well as an earthquake depth density map and fault density map. The overlaid data of these three maps onto ground acceleration map are then (compiled) to obtain an earthquake unit map. Some districts area, such as Sarmi, Nabire, and Dogiyai, are identified by a high vulnerability index. In the other hand, Waropen, Puncak, Merauke, Asmat, Mappi, and Bouven Digoel area shows lower index. Finally, the vulnerability index in other places is detected as moderate.

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Analysis of Mw 7.2 2014 Molucca Sea earthquake and its aftershocks

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AIP Conference Proceedings 2016年第1期1730卷

作者： Hasbi Ash Shiddiqi Sri Widiyantoro Andri Dian Nugraha Mohamad Ramdhan Samsul Hadi Wiyono Wandono Wandono 1Study Program of Earth Sciences Institute of Technology Bandung Indonesia 2Global Geophysics Research Group Faculty of Mining and Petroleum Engineering Institute of Technology Bandung Indonesia 3Meteorological Climatological and Geophysical Agency of Indonesia Jl. Angkasa 1 No. 2 Kemayoran Jakarta Indonesia

A Mw 7.2 earthquake struck an area in the Molucca Sea region on November 15, 2014, and was followed by more than 300 aftershocks until the end of December 2014. This earthquake was the second largest event in the Molucca Sea during the last decade and was well recorded by local networks. Although the seismicity rate of the aftershocks was declining at the end of 2014, several significant earthquakes with magnitude (Mw) larger than five still occurred from January to May 2015 within the vicinity of the mainshock location. In this study, we investigated the earthquake process and its relation to the increasing seismicity in the Molucca Sea within six months after the earthquake. We utilized teleseismic double-difference hypocenter relocation method using local, regional, and teleseismic direct body-wave arrival times of 514 earthquakes from the time of mainshock occurrence to May 2015. Furthermore, we analyzed the focal mechanism solutions from the National Research Institute for Earth Science and Disaster Prevention (NIED), Japan. From our results, we observed that aftershocks propagated along the NNE-SSW direction within a 100 km fault segment length of the Mayu Ridge. The highest number of the aftershocks was located in the SSW direction of the main event. The aftershocks were terminated at around 60 km depth, which may represent the location of the top of the Molucca Sea Plate (MSP). Between January and May 2015, several significant earthquakes propagated westward and were extended to the Molucca Sea slab. From focal mechanism catalog, we found that the mainshock mechanism was reverse with strike 192o and dip 55o. While most of the large aftershock mechanisms were consistent with the main event, several aftershocks had reverse, oblique mechanisms. Stress inversion result from focal mechanism data revealed that the maximum stress direction was SE and was not perpendicular with fault direction. We suggest that the non-perpendicular maximum stress caused several afte

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Observation of seismicity based on DOMERAPI and BMKG seismic networks: A preliminary result from DOMERAPI project

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AIP Conference Proceedings 2016年第1期1730卷

作者： Mohamad Ramdhan Andri Dian Nugraha Sri Widiyantoro Said Kristyawan Andry Syaly Sembiring Jean-Philippe Mtaxian 1Study Program of Earth Sciences Institute of Technology Bandung Indonesia 2Meteorological Climatological and Geophysical Agency of Indonesia Jl. Angkasa 1 No. 2 Kemayoran Jakarta Indonesia 3Global Geophysics Research Group Faculty of Mining and Petroleum Engineering Institute of Technology Bandung Indonesia 4Institut de Recherche pour le Dveloppement (IRD) France

DOMERAPI project has involved earth scientists from Indonesia and France to conduct comprehensively a study of the internal structure of Mt. Merapi and its vicinity based on seismic tomographic imaging. The DOMERAPI seismic network was running from October 2013 to April 2015 consisting of 53 broad-band seismometers, covering Mt. Merapi and Mt. Merbabu, and some geological features such as Opak and Dengkeng faults. Earthquake hypocenter determination conducted in this study is an important step before seismic tomographic imaging. The earthquake events were identified and picked manually and carefully. The majority of earthquakes occured outside the DOMERAPI network. The ray paths of seismic waves from these earthquakes passed through the deep part of the study area around Merapi. The joint data of BMKG and DOMERAPI networks can minimize the azimuthal gap, which is often used to obtain an indication of the reliability of the epicentral solution. Our preliminary results show 279 events from October 2013 to mid August 2014. For future work, we will incorporate the BPPTKG (Center for Research and Technology Development of Geological Disaster) data catalogue in order to enrich seismic ray paths. The combined data catalogues will provide information as input for further advanced studies and volcano hazards mitigation.

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Seismicity studies at Moluccas area based on the result of hypocenter relocation using HypoDD

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AIP Conference Proceedings 2015年第1期1658卷

作者： Muhammad Reza July Utama Andri Dian Nugraha Nanang T. Puspito 1Student of Geophysical Engineering Study Program Institute of Technology Bandung Indonesia 2Indonesian Meteorological Climatological and Geophysical Agency (MCGA) Jakarta Indonesia 3Global Geophysical Research Group Faculty of Mining and Petroleum Engineering ITB Indonesia

The precise hypocenter was determined location using double difference method around subduction zone in Moluccas area eastern part of Indonesia. The initial hypocenter location from MCGA data catalogue of 1,945 earthquake events. Basically the principle of double-difference algorithm assumes if the distance between two earthquake hypocenter distribution is very small compared to the distance between the station to the earthquake source, the ray path can be considered close to both earthquakes. The results show the initial earthquakes with a certain depth (fix depth 10 km) relocated and can be interpreted more reliable in term of seismicity and geological setting. The relocation of the intra slab earthquakes beneath Banda Arc are also clearly observed down to depth of about 400 km. The precise relocated hypocenter will give invaluable seismicity information for other seismological and tectonic studies especially for seismic hazard analysis in this region.

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Preliminary result of P-wave speed tomography beneath North Sumatera region

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AIP Conference Proceedings 2015年第1期1658卷

作者： Jajat Jatnika Andri Dian Nugraha Wandono Earth Science Study Program Institute of Technology Bandung Indonesia Indonesian Meteorological Climatological and Geophysical Agency MCGA Jakarta Indonesia Global Geophysical Research Group Faculty of Mining and Petroleum Engineering Insitute of Technology Bandung Indonesia

The structure of P-wave speed beneath the North Sumatra region was determined using P-wave arrival times compiled by MCGA from time periods of January 2009 to December 2012 combining with PASSCAL data for February to May 1995. In total, there are 2,246 local earthquake events with 10,666 P-wave phases from 63 stations seismic around the study area. Ray tracing to estimate travel time from source to receiver in this study by applying pseudo-bending method while the damped LSQR method was used for the tomographic inversion. Based on assessment of ray coverage, earthquakes and stations distribution, horizontal grid nodes was set up of 30×30 km2 for inside the study area and 80×80 km2 for outside the study area. The tomographic inversion results show low Vp anomaly beneath Toba caldera complex region and around the Sumatra Fault Zones (SFZ). These features are consistent with previous study. The low Vp anomaly beneath Toba caldera complex are observed around Mt. Pusuk Bukit at depths of 5 km down to 100 km. The interpretation is these anomalies may be associated with ascending hot materials from subduction processes at depths of 80 km down to 100 km. The obtained Vp structure from local tomography will give valuable information to enhance understanding of tectonic and volcanic in this study area.

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