Pull-apart basin formation and development in narrow transform zones with application to the Dead Sea Basin

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Pull-apart basin formation and development in narrow transform zones with application to the Dead Sea Basin

[1] Contrary to other examples, like Death Valley, California, and the Sea of Marmara, Turkey, the Dead Sea-type pull-apart basins form within a narrow transform corridor between strike-slip faults that are less than 10 km apart, much smaller than the crustal thickness of 35 km. In this paper we investigate the role of fault zone width versus thickness and rheology on the mechanics of pull-apar...

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Mount Sedom is the surface expression of a salt diapir that has emerged since the Pleistocene in the southwestern part of the Dead Sea basin. Milestones in the uplift history of the Sedom salt diapir since its inception were deduced from angular and erosional unconformities, thickness variations, caprock formation, chemistry and isotope composition of lacustrine aragonite, cave morphology, prec...

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ژورنال

عنوان ژورنال: Tectonics

سال: 2008

ISSN: 0278-7407

DOI: 10.1029/2007tc002119