Titlebook: Dead Sea Transform Fault System: Reviews; Zvi Garfunkel,Zvi Ben-Avraham,Elisa Kagan Book 2014 Springer Science+Business Media Dordrecht 20

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,The Story of Saline Water in the Dead Sea Rift – The Role of Runoff and Relative Humidity,he south. The maximum salinity of the waters reaches 340 g L., and their chemical composition is Ca-chloridic, like most subsurface brines in sedimentary basins elsewhere. It is now generally accepted that such waters evolved from ancient seawater via a three-stage mechanism, namely: (1) seawater ev

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https://doi.org/10.1007/978-3-031-65960-7eral and estimated at approximately 5–7 mm/year. The fault is seismically active. The extensional regime combined with the dominant lateral motion along the DSF resulted in the formation of a series of deep pull-apart basins. These basins are among the largest and deepest in the world. The crustal s

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Meryem Altaf,Nosheen Jawaid Khanbrated by geological and geodynamic evidence..We use seismics, seismology and gravity to study the crust and lithosphere of the Dead Sea Transform (DST) system. These observations are integrated with 3D thermo-mechanical modelling of the evolution of the DST through time to understand the deeper str

finite

Meryem Altaf,Nosheen Jawaid Khand possibly as deep as 33.6 km. From these distributions, the seismogenic thickness is estimated to be 28.4 ± 2.2 km. The existence of a seismogenic zone extending deep into the lower crust is consistent with an average heat flow of only 40–45 mWm. over most regions of Israel, and around 40 mWm. in t

MINT

https://doi.org/10.1007/978-3-031-51862-1 that this tectono-magmatic association has mainly to do with the magma migration toward the surface and less with magma generation, namely: some volcanic activity concentrated along the DST due to better magma channeling and not due to an enhanced mantle partial melting along this lineament. The vo

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Sublingual Salivary Gland Abnormalities,these studies include: the determination of slip rate of the DSF across different space and time resolutions, which converges at around 4–5 mm/a, confirmation of the sinistral relative motion between the Arabia Plate and the Sinai Subplate and of thrust motion and normal faulting associated with res

hypnogram

Martin Giera,Elena Sánchez-Lópezaeological sites, disturbed beds in lake deposits, rockfalls within caves as well as on free slopes, and displaced marine terraces. The rich historical archive is useful as a key for deciphering the geological archives..Of the geological archives developed for the Dead Sea rift, lake sections stand

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