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- W2184700429 abstract "Fractures and fault zones are studied in the Dead Sea Rift with geological and structural methods. As is established from the statistical processing of the data, the N-S- and NW-trending faults control the struc- ture in the southern portion of this rift. They are the longest and accompanied by the thickest crush zones and the most developed fracture systems in comparison with faults oriented in other directions. The roughly merid- ional trend of fracture systems is vividly expressed within basins and often shaded by other fracture systems in the interbasin links. Mesostructural marks indicate the normal faulting along master faults within local basins, while between them, in uplifted offsets, the displacements may change from normal to strike-slip within the same fault zone. The NW-trending faults are characterized by normal and combined normal and strike-slip dis- placements; the E-W faults reveal lateral displacement, and the NE-trending faults exhibit strike-slip and nor- mal displacements. Two local stress fields equal in implications for the tectonic evolution of the Dead Sea Rift have been reconstructed from the fracture patterns: (1) E-W (predominant) and ENE extension and (2) shear accompanied by the NE or less developed E-W extension and the NW or less developed N-S compression. Com- parison of the results obtained with analog models of structural systems formed under various loading conditions shows that the specific features of faulting and stress fields in the Dead Sea Rift resulted from oblique extension." @default.
- W2184700429 created "2016-06-24" @default.
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- W2184700429 date "2005-01-01" @default.
- W2184700429 modified "2023-09-27" @default.
- W2184700429 title "Fault Systems and Stress Fields in the Southern Dead Sea Rift" @default.
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