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Nanang T. Puspito

Researcher at Bandung Institute of Technology

Publications -  72
Citations -  754

Nanang T. Puspito is an academic researcher from Bandung Institute of Technology. The author has contributed to research in topics: Hypocenter & Subduction. The author has an hindex of 10, co-authored 65 publications receiving 578 citations. Previous affiliations of Nanang T. Puspito include University of Tokyo.

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Tsunami Catalog and Zones in Indonesia

TL;DR: In this paper, the histograms of earthquakes and tsunami by region by decade from 1600 to 1999 were made, based on data compiled during the period 1600-1999, 105 tsunami have occurred in Indonesia, 90% of them were caused by earthquakes in a shallow region at subduction and plate boundaries, 9% by volcanic eruption, and 1% by a landslide.
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P and S velocity structure of the crust and the upper mantle beneath central Java from local tomography inversion

TL;DR: In this article, the results of local source tomographic inversion are presented for central Java, showing that a double seismic zone is observed in the slab between 80 and 150 km depth, and the most striking feature of the resulting P and S models is a pronounced low-velocity anomaly in the crust, just north of the volcanic arc.
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Early detection of drought impact on rice paddies in Indonesia by means of Niño 3.4 index

TL;DR: In this paper, the authors developed the Paddy Drought Impact Index (PDII), which is the ratio of drought-induced paddy damaged area to the total paddy area planted in order to investigate the impact of drought on paddies among 335 districts in Indonesia.
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Mantle structure and seismotectonics of the Sunda and Banda arcs

TL;DR: In this article, the authors examined the mantle structure and seismotectonic features of the Sunda and Banda arcs, Indonesia, based on the P-wave tomographic images, focal mechanism solutions, gravity anomaly and heat-flow data.
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Three-dimensional P-wave velocity structure beneath the Indonesian region

TL;DR: In this article, the authors presented the P-wave seismic tomography image of the mantle to a depth of 1200 km beneath the Indonesian region, where the artb inversion method was applied to a dataset of 118,203 Pwave travel times of local and teleseismic events taken from ISC bulletins.