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Nugroho D. Hananto

Researcher at Indonesian Institute of Sciences

Publications -  49
Citations -  1409

Nugroho D. Hananto is an academic researcher from Indonesian Institute of Sciences. The author has contributed to research in topics: Subduction & Forearc. The author has an hindex of 16, co-authored 48 publications receiving 1212 citations. Previous affiliations of Nugroho D. Hananto include Institut de Physique du Globe de Paris.

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Supporting Online Material for Deformation and Slip Along the Sunda Megathrust in the Great 2005 Nias-Simeulue Earthquake

TL;DR: Measurements from coral microatolls and Global Positioning System stations reveal trench-parallel belts of uplift up to 3 meters high on the outer-arc islands above the rupture and a 1-meter-deep subsidence trough farther from the trench.
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Deformation and Slip Along the Sunda Megathrust in the Great 2005 Nias-Simeulue Earthquake

TL;DR: The Sunda-Andaman megathrust deformation has been studied from coral microatolls and Global Positioning System (GPS) data in this paper, which reveals trench-parallel belts of uplift up to 3 meters high on the outer arc islands above the rupture and a 1-meter-deep subsidence trough farther from the trench.
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Seismic evidence for broken oceanic crust in the 2004 Sumatra earthquake epicentral region

TL;DR: In this paper, the authors present a high-quality seismic section of the focal region, from the abyssal plain down to 40'km depth below the fore-arc, showing that the subducting crust and oceanic Moho are broken and displaced by landward-dipping thrust ramps, suggesting that the megathrust now lies in the oceanic mantle.
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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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Evidence of active backthrusting at the NE Margin of Mentawai Islands, SW Sumatra

TL;DR: Using a combination of high-resolution seismic reflection and bathymetry data, this paper showed that the Mentawai Fault seems to be characterized by active SW dipping backthrusts.