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M. Ma’ruf Mukti

Researcher at Indonesian Institute of Sciences

Publications -  33
Citations -  349

M. Ma’ruf Mukti is an academic researcher from Indonesian Institute of Sciences. The author has contributed to research in topics: Forearc & Subduction. The author has an hindex of 7, co-authored 30 publications receiving 279 citations. Previous affiliations of M. Ma’ruf Mukti include Institut de Physique du Globe de Paris & Chiba University.

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Aseismic zone and earthquake segmentation associated with a deep subducted seamount in Sumatra

TL;DR: In this paper, a seamount subducted to 40 km depth below Sumatra was associated with an aseismic zone, suggesting that at this location, the seamount reduces coupling of the slab and overriding plate.
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Seismic images of structural variations along the deformation front of the Andaman???Sumatra subduction zone: Implications for rupture propagation and tsunamigenesis

TL;DR: In this article, seven deep seismic reflection profiles cover the 3000 km-long subduction system from Andaman to Southern Sumatra, including zones that ruptured in 2004, 2007, and 2010.
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Seismic images of the megathrust rupture during the 25th October 2010 Pagai earthquake, SW Sumatra: Frontal rupture and large tsunami

TL;DR: In this paper, the authors present seismic reflection and bathymetry images from the 2010 epicentral region acquired before the earthquake, and find that the frontal thrust is the main active fault in this region and might have ruptured up to the seafloor at 6 km water depth uplifting the water column and producing a large tsunami.
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Structural evolution of backthrusting in the Mentawai Fault Zone, offshore Sumatran forearc

TL;DR: In this paper, the authors presented the interpretation of newly acquired high-quality industry-standard deep seismic reflection and swath bathymetry data to provide insight into the structural style and evolution of the Mentawai Fault Zone (MFZ).
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The use of microstructures for discriminating turbiditic and hemipelagic muds and mudstones

TL;DR: In this paper, the microstructures of turbiditic and hemipelagic muds and mudstones were investigated using a scanning electron microscope to determine whether there are microstructural features that can differentiate turbidite from hemipelagous sedimentary processes.