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- W2802542909 abstract "Speculations surround salt deformation in the Mediterranean Basins, both related to the deformation history and the triggers for halokinesis since the onset of the Messinian Salinity Crisis. This work presents a detailed description of the mechanisms driving internal and external deformation of a salt giant from the Levant Basin, offshore Israel. The intrasalt siliciclastic layers generate good internal reflectivity within the Messinian evaporites, allowing a thorough elucidation of the complex evolution and nature of syn-Messinian and post-Messinian structures. We have identified three distinct phases of deformation in the deep basin, based on the orientation, timing, and geometry of their related structures: The first phase is characterized by small-scaled, gravity-driven, contractional faults and folds oriented N-S that have been overprinted by a second syn-Messinian, NW-SE trending, deformation phase affecting the clastic bundles. This latter deformation phase is the cause of truncation of the intrasalt stringers on the intra-Messinian truncation surface. The third deformation phase occurred in the Pleistocene and affected all strata from the Messinian salt to the seabed. This deformational phase produced thrust, strike-slip, and normal faults, but the dominant orientation of the thrust faults and folds is NNW-SSE. Our study demonstrates that the first deformation phase was caused by regional uplift along the Levant margin during the Messinian, the second is a response to basin subsidence toward the Cyprus Arc, also syn-Messinian, and the third phase is likely related to the reorganization of the African-Eurasian plate boundary and activity along the Dead Sea Transform after the Messinian Salinity Crisis." @default.
- W2802542909 created "2018-05-17" @default.
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- W2802542909 date "2018-05-01" @default.
- W2802542909 modified "2023-10-01" @default.
- W2802542909 title "Multiphase Structural Evolution and Geodynamic Implications of Messinian Salt-Related Structures, Levant Basin, Offshore Israel" @default.
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- W2802542909 cites W1947809444 @default.
- W2802542909 cites W1964702838 @default.
- W2802542909 cites W1970313428 @default.
- W2802542909 cites W1973309627 @default.
- W2802542909 cites W1980417494 @default.
- W2802542909 cites W1982666117 @default.
- W2802542909 cites W1989072731 @default.
- W2802542909 cites W1990900345 @default.
- W2802542909 cites W1991468612 @default.
- W2802542909 cites W1996188539 @default.
- W2802542909 cites W1997583625 @default.
- W2802542909 cites W1999165622 @default.
- W2802542909 cites W2003820922 @default.
- W2802542909 cites W2009463099 @default.
- W2802542909 cites W2019139651 @default.
- W2802542909 cites W2019967542 @default.
- W2802542909 cites W2023989753 @default.
- W2802542909 cites W2024073935 @default.
- W2802542909 cites W2025296492 @default.
- W2802542909 cites W2027848502 @default.
- W2802542909 cites W2029075053 @default.
- W2802542909 cites W2032123209 @default.
- W2802542909 cites W2033804660 @default.
- W2802542909 cites W2035455313 @default.
- W2802542909 cites W2040964459 @default.
- W2802542909 cites W2040989064 @default.
- W2802542909 cites W2046620296 @default.
- W2802542909 cites W2054014017 @default.
- W2802542909 cites W2054917917 @default.
- W2802542909 cites W2055344849 @default.
- W2802542909 cites W2057524081 @default.
- W2802542909 cites W2058664810 @default.
- W2802542909 cites W2058788458 @default.
- W2802542909 cites W2059777175 @default.
- W2802542909 cites W2072621765 @default.
- W2802542909 cites W2076258856 @default.
- W2802542909 cites W2077639299 @default.
- W2802542909 cites W2082213466 @default.
- W2802542909 cites W2085327403 @default.
- W2802542909 cites W2086738712 @default.
- W2802542909 cites W2091888047 @default.
- W2802542909 cites W2092093635 @default.
- W2802542909 cites W2099970799 @default.
- W2802542909 cites W2110039350 @default.
- W2802542909 cites W2117032570 @default.
- W2802542909 cites W2118326191 @default.
- W2802542909 cites W2120857027 @default.
- W2802542909 cites W2132418823 @default.
- W2802542909 cites W2132926881 @default.
- W2802542909 cites W2133346363 @default.
- W2802542909 cites W2137820648 @default.
- W2802542909 cites W2142644050 @default.
- W2802542909 cites W2148135691 @default.
- W2802542909 cites W2150238921 @default.
- W2802542909 cites W2151250266 @default.
- W2802542909 cites W2153276776 @default.
- W2802542909 cites W2154592894 @default.
- W2802542909 cites W2155228051 @default.
- W2802542909 cites W2161667391 @default.
- W2802542909 cites W2263887095 @default.
- W2802542909 cites W2316943139 @default.
- W2802542909 cites W2317723920 @default.
- W2802542909 cites W2323171794 @default.
- W2802542909 cites W2460629409 @default.
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- W2802542909 doi "https://doi.org/10.1029/2017tc004794" @default.
- W2802542909 hasPublicationYear "2018" @default.
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