Geodynamics of Sumatra is interesting to study because of the unique geological setting and high seismicity. This high seismicity is caused by the many faults found on land and in the surrounding waters. This paper presents the results of research that aims to determine fault patterns both on land and in the waters around Sumatra based on earthquake data from 1960-2000. The area under study is at the coordinates of 6°N - 6°S and 95°E - 109°E at an epicenter depth of <60 km with a magnitude between 4-10. The area is divided into two zones, namely the front arc and the Barisan arc. Data were obtained from ISC and Global CMT. By using the Focal Mechanism Method, the results show that the fault pattern in the Sumatran forearc Basin zone is domi...
Fifteen earthquakes (Mw 4.1-6.4) occurring at ten major segments of the Sumatran Fault Zone (SFZ) we...
[1] The combination of the Sunda megathrust and the (strike-slip) Sumatran Fault (SF) represents a t...
DOI: 10.17014/ijog.5.2.137-160A detailed active fault study in Tarutung-Sarulla-Sipirok-Padangsidemp...
Geodynamics of Sumatra is interesting to study because of the unique geological setting and high sei...
Natural hazards that are affecting humans are mostly related to geological processes, for example ea...
© 2018 by the authors. Licensee MDPI, Basel, Switzerland. Located approximately a hundred kilometres...
Located approximately a hundred kilometres north of Java Subduction Zone, Java Island has a complica...
INDONESIA: Sumatra salah satu pulau terbesar di Indonesia yang memiliki potensi rawan b...
Sumatran Fault is one of hazard located in Sumatra Island. Southern segment of Sumatran fault is one...
Large subduction earthquakes have repeatedly occurred along the Sumatra subduction zone, where the A...
Indonesia is the meeting zone between three world main plates: Eurasian Plate, Pacific Plate, and In...
Kota Baru, a new capital Lampung province location, planned and developed since 2012, will be a dens...
Kota Baru, a new capital Lampung province location, planned and developed since 2012, will be a dens...
Five earthquakes source parameters in Sumatra have been estimated that occurred on May 3rd, 13th , 1...
To help with efforts to mitigate earthquake hazards, we need to understand how faults have behaved i...
Fifteen earthquakes (Mw 4.1-6.4) occurring at ten major segments of the Sumatran Fault Zone (SFZ) we...
[1] The combination of the Sunda megathrust and the (strike-slip) Sumatran Fault (SF) represents a t...
DOI: 10.17014/ijog.5.2.137-160A detailed active fault study in Tarutung-Sarulla-Sipirok-Padangsidemp...
Geodynamics of Sumatra is interesting to study because of the unique geological setting and high sei...
Natural hazards that are affecting humans are mostly related to geological processes, for example ea...
© 2018 by the authors. Licensee MDPI, Basel, Switzerland. Located approximately a hundred kilometres...
Located approximately a hundred kilometres north of Java Subduction Zone, Java Island has a complica...
INDONESIA: Sumatra salah satu pulau terbesar di Indonesia yang memiliki potensi rawan b...
Sumatran Fault is one of hazard located in Sumatra Island. Southern segment of Sumatran fault is one...
Large subduction earthquakes have repeatedly occurred along the Sumatra subduction zone, where the A...
Indonesia is the meeting zone between three world main plates: Eurasian Plate, Pacific Plate, and In...
Kota Baru, a new capital Lampung province location, planned and developed since 2012, will be a dens...
Kota Baru, a new capital Lampung province location, planned and developed since 2012, will be a dens...
Five earthquakes source parameters in Sumatra have been estimated that occurred on May 3rd, 13th , 1...
To help with efforts to mitigate earthquake hazards, we need to understand how faults have behaved i...
Fifteen earthquakes (Mw 4.1-6.4) occurring at ten major segments of the Sumatran Fault Zone (SFZ) we...
[1] The combination of the Sunda megathrust and the (strike-slip) Sumatran Fault (SF) represents a t...
DOI: 10.17014/ijog.5.2.137-160A detailed active fault study in Tarutung-Sarulla-Sipirok-Padangsidemp...