Temporal variation in the geometry of a strike–slip fault zone: Examples from the Dead Sea Transform

The location of the active fault strands along the Dead Sea Transform fault zone (DST) changed through time. In the western margins of Dead Sea basin, the early activity began a few kilometers west of the preset shores and moved toward the center of the basin in four stages. Similar centerward migra...

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Veröffentlicht in:	Tectonophysics 2007-12, Vol.445 (3), p.186-199
1. Verfasser:	Marco, Shmuel
Format:	Artikel
Sprache:	eng
Schlagworte:	Active faulting Dead Sea Transform fault Fault segmentation Fault zone geometry Middle East Tectonics
Online-Zugang:	Volltext
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