scispace - formally typeset
K

K. H. Palgunadi

Researcher at King Abdullah University of Science and Technology

Publications -  21
Citations -  129

K. H. Palgunadi is an academic researcher from King Abdullah University of Science and Technology. The author has contributed to research in topics: Aftershock & Fault (geology). The author has an hindex of 4, co-authored 16 publications receiving 56 citations. Previous affiliations of K. H. Palgunadi include Bandung Institute of Technology & Institut de Physique du Globe de Paris.

Papers
More filters
Journal ArticleDOI

Dynamic fault interaction during a fluid-injection induced earthquake: The 2017 Mw 5.5 Pohang event

TL;DR: In this article, the authors conduct a 3D high-resolution spontaneous dynamic rupture simulation of an induced earthquake and identify a main and a secondary fault plane that intersects under a shallow angle of 15°.
Journal ArticleDOI

Hypocenter relocation of the aftershocks of the Mw 7.5 Palu earthquake (September 28, 2018) and swarm earthquakes of Mamasa, Sulawesi, Indonesia, using the BMKG network data

TL;DR: In this article, the authors used the double-difference relocation method (hypoDD) to relocate 386 of the 554 Palu aftershocks by using the double difference relocation method from September 28 to November 22, 2018.
Journal ArticleDOI

Methodology for Full Waveform Near Real-Time Automatic Detection and Localization of Microseismic Events Using High (8 kHz) Sampling Rate Records in Mines: Application to the Garpenberg Mine (Sweden)

TL;DR: In this paper, the first author was a student of the Paris Exploration Geophysics Group program (GPX), funded by the French National Research Agency (ANR), Compagnie Generale de Geophysique (CGG), TOTAL, and Schlumberger.
Journal ArticleDOI

Seismic repeaters linked to weak rock-mass creep in deep excavation mining

TL;DR: In this paper, the authors show that seismic repeaters represent brittle frictional parts (asperity) of creeping, planar shaped, pre-exiting structures of several metres composed of weak rock-mass materials (e.g. talc) associated with strengthening friction behaviours.