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

容易做

Lateral Motion and Deformation Along the Dead Sea Transform,thinned and may have been intruded by basalts. The structural pattern changed over time, the present pattern having been mostly established in the second half of the DST history. North of lat. ca. 33°N transpression dominates and the DST flanks are strongly deformed by folding, faulting, and rotatio

FRAX-tool

Pleistocene Strain Partitioning During Transpression Along the Dead Sea Transform, Metulla Saddle, oundary zone, including nearly vertical fault planes, horizontal striae, alternating throw from one side of the fault to the other, and an assemblage of en-echelon folds and “positive flower structures”. Kinematic analysis of fault data and principal AMS axes reveals strain axes, which are compatibl

典型

Review of On-Fault Palaeoseismic Studies Along the Dead Sea Fault,erm rate of seismicity is not necessarily representative of the long-term seismic activity along the DSF. Assuming the historical records of the last two millennia are complete for strong earthquakes, we note long periods of quiescence in the sections of the northern Yammouneh, the Jordan Valley, an

CRACY

Pre-Instrumental Earthquakes Along the Dead Sea Rift,ive..The historical information spans periods that exceed the seismic cycle of individual fault segments. One of the provoking results of the comparisons of historical versus geological archives of earthquake activity is the significant difference in the apparent length of the earthquake cycle, wher

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Gum-Disease

The Evolution of Neogene-Quaternary Water-Bodies in the Dead Sea Rift Valley,story of the water-bodies. The chronologies are mainly based on U-series, radiocarbon and oxygen isotope stratigraphy methods and provide the base for detailed geochemical and sedimentological reconstruction of the limnological-hydrological conditions in the watershed. The solutions that filled the

Organization

,The Story of Saline Water in the Dead Sea Rift – The Role of Runoff and Relative Humidity, salt bodies; indeed, such were actually found in the subsurface of the two tectonic depressions of the Dead Sea and Lake Kinneret (Sea of Galilee). It is likely that the ancient lagoon from which the seawater evaporated and in which the salt deposited was approximately 300 km long and 20 km wide..T

簡略

1876-1682 ased on recent studies of the tectonics, structure, geophysics, volcanism, active tectonics, sedimentology and paleo and modern climate of the Dead Sea transform fault zone. It puts together all this new information and knowledge in a coherent fashion..978-94-024-0514-9978-94-017-8872-4Series ISSN 1876-1682 Series E-ISSN 1876-1690

Multiple

https://doi.org/10.1007/978-3-031-65960-7ther in contexts of various geophysical properties, and discussing their tectonic implications. A simulation of faulting processes along the northern DSF and the Levant margin suggested that the formation of the DSF could be explained as a result of simultaneous propagation from the north and south.

鉆孔

Meryem Altaf,Nosheen Jawaid Khanaba Fault (AF). In the Dead Sea Basin (DSB) proper the imaging of the Moho is complicated by the presence of the Lisan Salt dome. From these results and other evidence we conclude that the Dead Sea basin is a mostly upper crustal feature with a decoupling zone at about 20 km depth. Using SKS waves w