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[PDF] Top 20 Calculation of coseismic displacement from lidar data in the 2016 Kumamoto, Japan, earthquake

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Calculation of coseismic displacement from lidar data in the 2016 Kumamoto, Japan, earthquake

Calculation of coseismic displacement from lidar data in the 2016 Kumamoto, Japan, earthquake

... It is not necessary to calculate the correlation for all the locations because it requires unnecessary computational ef- forts. A better procedure is to move the post-event window along the direction in which the ... See full document

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Detection of collapsed buildings from lidar data due to the 2016 Kumamoto earthquake in Japan

Detection of collapsed buildings from lidar data due to the 2016 Kumamoto earthquake in Japan

... the Kumamoto earthquake sequence where significant permanent ground displacements were produced during the ...(3-D) displacement was imple- mented. The permanent ground displacement was ... See full document

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Characteristics of the surface ruptures associated with the 2016 Kumamoto earthquake sequence, central Kyushu, Japan

Characteristics of the surface ruptures associated with the 2016 Kumamoto earthquake sequence, central Kyushu, Japan

... of Japan 2016e) ...Napa earthquake of August 24, 2014 (Bray et ...the Kumamoto earthquake were documented along both the Hinagu and Futagawa fault zones by geodetic surveys such as InSAR ... See full document

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Source location and mechanism analysis of an earthquake triggered by the 2016 Kumamoto, southwestern Japan, earthquake

Source location and mechanism analysis of an earthquake triggered by the 2016 Kumamoto, southwestern Japan, earthquake

... for calculation of the synthetic waveform are unknown and are not estimated in this ...waves from the mainshock into the com- ...s from the arrival time of ... See full document

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Numerical simulations to explain the coseismic electromagnetic signals: a case study for a M5 4 aftershock of the 2016 Kumamoto earthquake

Numerical simulations to explain the coseismic electromagnetic signals: a case study for a M5 4 aftershock of the 2016 Kumamoto earthquake

... started from daytime (in JST) on April 14, 2016; meanwhile the mainshock of the Kumamoto earthquake occurred at 01:25 (in JST) on April 16, ...EM data were acquired until daytime (in ... See full document

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Geomorphic features of surface ruptures associated with the 2016 Kumamoto earthquake in and around the downtown of Kumamoto City, and implications on triggered slip along active faults

Geomorphic features of surface ruptures associated with the 2016 Kumamoto earthquake in and around the downtown of Kumamoto City, and implications on triggered slip along active faults

... 7.3) earthquake at 01:25 JST on April 16 in Kuma- moto Prefecture appeared along the previously mapped ~100-km-long active fault called the Futagawa-Hinagu fault zone ...of Japan (GSI) indicated ... See full document

12

The cause of heavy damage concentration in downtown Mashiki inferred from observed data and field survey of the 2016 Kumamoto earthquake

The cause of heavy damage concentration in downtown Mashiki inferred from observed data and field survey of the 2016 Kumamoto earthquake

... 16, 2016) of the 2016 Kuma- moto earthquake sequence, we carried out a field survey from April 29 through May 1, 2016, in Mashiki where heavy damage concentration was ...the ... See full document

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Underground structures associated with horizontal sliding at Uchinomaki hot springs, Kyushu, Japan, during the 2016 Kumamoto earthquake

Underground structures associated with horizontal sliding at Uchinomaki hot springs, Kyushu, Japan, during the 2016 Kumamoto earthquake

... DInSAR data to have been displaced to the northwest (Tsuji et ...greatest displacement in the study area (location B in ...to earthquake vibration (i.e., dynamic stress during the earthquake) ... See full document

9

Source rupture processes of the foreshock and mainshock in the 2016 Kumamoto earthquake sequence estimated from the kinematic waveform inversion of strong motion data

Source rupture processes of the foreshock and mainshock in the 2016 Kumamoto earthquake sequence estimated from the kinematic waveform inversion of strong motion data

... The 2016 Kumamoto earthquake sequence started with an M JMA ...Kyushu, Japan, and the M JMA ...started from the deep portion of a northwest-dipping fault plane along the northern part ... See full document

11

Bayesian inference and interpretation of centroid moment tensors of the 2016 Kumamoto earthquake sequence, Kyushu, Japan

Bayesian inference and interpretation of centroid moment tensors of the 2016 Kumamoto earthquake sequence, Kyushu, Japan

... acceleration data (K-NET and KiK-net) and strong motion velocity data corrected for the instrument response (F-net) are filtered by a bandpass filter and integrated into displacements (the K-NET and KiK-net ... See full document

19

Landslides triggered by an earthquake and heavy rainfalls at Aso volcano, Japan, detected by UAS and SfM-MVS photogrammetry

Landslides triggered by an earthquake and heavy rainfalls at Aso volcano, Japan, detected by UAS and SfM-MVS photogrammetry

... topographic data for geoscientific ...of coseismic landslides triggered by the 2016 Kumamoto earthquake (Mw ...the 2016 Kumamoto ...54 coseismic landslides with ... See full document

10

Fault source model for the 2016 Kumamoto earthquake sequence based on ALOS 2/PALSAR 2 pixel offset data: evidence for dynamic slip partitioning

Fault source model for the 2016 Kumamoto earthquake sequence based on ALOS 2/PALSAR 2 pixel offset data: evidence for dynamic slip partitioning

... in Kumamoto prefecture in the middle of the Kyushu island, ...ALOS-2/PALSAR-2 data covering three M w > 6 earthquakes and derived the 3D displacements around the ...trending displacement ... See full document

10

Anomalous decrease in relatively large shocks and increase in the p and b values preceding the April 16, 2016, M7 3 earthquake in Kumamoto, Japan

Anomalous decrease in relatively large shocks and increase in the p and b values preceding the April 16, 2016, M7 3 earthquake in Kumamoto, Japan

... 1894). From the view point of the rate- and state-dependent fric- tion law (Dieterich 1994), variability in p can be observed: p > 1 and p < 1 for rapidly and slowly decreasing stress, ... See full document

8

Simultaneous estimation of the dip angles and slip distribution on the faults of the 2016 Kumamoto earthquake through a weak nonlinear inversion of InSAR data

Simultaneous estimation of the dip angles and slip distribution on the faults of the 2016 Kumamoto earthquake through a weak nonlinear inversion of InSAR data

... the Kumamoto earthquake ...looking from ascending orbits, because these images cover the entire source region and give us different view of deformation from both east and ...InSAR data ... See full document

10

Surface fault ruptures associated with the 14 April foreshock (Mj 6 5) of the 2016 Kumamoto earthquake sequence, southwest Japan

Surface fault ruptures associated with the 14 April foreshock (Mj 6 5) of the 2016 Kumamoto earthquake sequence, southwest Japan

... hand, Earthquake Research Committee, Headquarters for Earthquake Research Promotion (ERC- HERP) (2016) regarded the Futagawa and Kita-Amagi faults as part of the Futagawa fault zone, and the Takano ... See full document

8

Slip partitioned surface ruptures for the Mw 7 0 16 April 2016 Kumamoto, Japan, earthquake

Slip partitioned surface ruptures for the Mw 7 0 16 April 2016 Kumamoto, Japan, earthquake

... undertaken from 16 April to 16 June by ~20 research scientists from numerous Japa- nese ...al. 2016), conclude that the surface rupture associated with the 16 April 2016 event is ~30 km long, ... See full document

11

Continuity, segmentation and faulting type of active fault zones of the 2016 Kumamoto earthquake inferred from analyses of a gravity gradient tensor

Continuity, segmentation and faulting type of active fault zones of the 2016 Kumamoto earthquake inferred from analyses of a gravity gradient tensor

... These derivatives work as a high-pass filter, which detect relatively shallow and detailed structures. HD evaluates horizontally steep gravity gradients. Therefore, HD is often used to detect faults and structural ... See full document

9

An investigation into the remote triggering of the Oita earthquake by the 2016 Mw 7 0 Kumamoto earthquake using full wavefield simulation

An investigation into the remote triggering of the Oita earthquake by the 2016 Mw 7 0 Kumamoto earthquake using full wavefield simulation

... the Japan Integrated Velocity Structure Model (Koketsu et ...the Kumamoto earthquake, we use the JMA CMT solution ...OIT009 from the 2016 Kumamoto earth- quake by using the SEISM ... See full document

8

Observation of earthquake ground motion due to aftershocks of the 2016 Kumamoto earthquake in damaged areas

Observation of earthquake ground motion due to aftershocks of the 2016 Kumamoto earthquake in damaged areas

... in Kumamoto city with some stations in Mashiki town for ...the Kumamoto plain have dominant peaks at periods of ...in Kumamoto basin including the nature of the above-mentioned later ... See full document

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Coseismic displacements of the 14 November 2016 Mw 7.8 Kaikoura, New Zealand, earthquake using the Planet optical cubesat constellation

Coseismic displacements of the 14 November 2016 Mw 7.8 Kaikoura, New Zealand, earthquake using the Planet optical cubesat constellation

... PlanetScope data for coseismic displacements is their anticipated daily ...potential displacement accuracy: variance of dis- placements over homogenously displacing areas using or- thorectified ... See full document

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