Hasanuddin Z. Abidin

TL;DR: Kinematic analysis of the GPS recordings indicates that the centroid of released deformation is located at least 200 km north of the seismological epicentre, and provides evidence that the rupture propagated northward sufficiently fast for stations in northern Thailand to have reached their final positions less than 10 min after the earthquake, ruling out the hypothesis of a silent slow aseismic rupture.

TL;DR: In this article, the authors show that the rupture plane for this earthquake must have been at least 1,000 km long and that non-homogeneous slip is required to fit the large displacement gradients revealed by the GPS measurements.

TL;DR: In this article, the authors found that the spatial and temporal variations of land subsidence depend on the corresponding variations of groundwater extraction, coupled with the characteristics of sedimentary layers and building loads above it.

TL;DR: In this article, the authors investigated the characteristics and pattern of land subsidence in the Jakarta area using data from three repeated leveling surveys performed in 1982, 1991, and 1997, and two repeated GPS surveys conducted in 1997 and 1999.

TL;DR: In this article, the authors characterize subsidence in the Jakarta basin using eight episodic/campaign GPS surveys between 1997 and 2005, and the estimated subsidence rates are 1-10 cm/year.