Haluk Eyidogan

TL;DR: In this article, the authors presented a synthesis of recent studies of active tectonics in the region, including inland and underwater observations, in order to have a critical appraisal of the existence of large seismic gaps in the central and eastern Marmara Sea.

TL;DR: In this paper, a model of the Erzincan basin is proposed, which combines a pull-apart on the North Anatolian Fault (NAF) with the effect of two compressional wedges.

TL;DR: In this article, Herrmann et al. presented a study that has been supported by INGV and by the Earthquake and Engineering Research Centers Program of the National Science Foundation under Award Number EEC-9701785.

TL;DR: In this paper, a field experiment carried out from 17 July to 2 November 1999 with a dense seismic network surrounding the Marmara Sea region and including the rupture zone of the Izmit (Kocaeli) destructive earthquake of 17 August 1999 (M W 7.6, Harvard centroid moment tensor); (Delouis et al., 2002) permitted the collection of precise seismic data and the quantitative evaluation of the associated set of surface ruptures.

TL;DR: The spatial distribution of aftershocks suggests that the Palu segment does not terminate to the east of Palu town but extends in the N50°E direction where it has produced a 30 km right stepover as discussed by the authors.