Shallow lithological structure across the Dead Sea Transform derived from geophysical experiments
نویسندگان
چکیده
منابع مشابه
Shallow architecture of the Wadi Araba fault (Dead Sea Transform) from high-resolution seismic investigations
In a high-resolution small-scale seismic experiment we investigated the shallow structure of the Wadi Araba fault (WAF), the principal fault strand of the Dead Sea Transform System between the Gulf of Aqaba/Eilat and the Dead Sea. The experiment consisted of 8 sub-parallel 1 km long seismic lines crossing the WAF. The recording station spacing was 5 m and the source point distance was 20 m. The...
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S.P. Flego, A. Plastino , and A.R. Plastino 4 Universidad Nacional de La Plata, Instituto de F́ısica (IFLP-CCT-CONICET), C.C. 727, 1900 La Plata, Argentina and Universitat de les Illes Balears and IFISC-CSIC, 07122 Palma de Mallorca, Spain Universidad Nacional de La Plata, Facultad de Ingenieŕıa, Depto. de Ciencias Básicas, 1900 La Plata, Argentina 3 CREG-University of La Plata-CONICET Instituto...
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_Abstract. Two major hypotheses have been advanced for the formation of the long wavelength (100-300 km) undulations of oceanic basement and overlying sediments developed in the central Indian Ocean basin: whole layer folding (buckling) and local thickening (inverse boudinage). Using appropriately scaled two-layer analogue models for the oceanic lithosphere comprising a brittle layer above a du...
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ژورنال
عنوان ژورنال: Geochemistry, Geophysics, Geosystems
سال: 2011
ISSN: 1525-2027
DOI: 10.1029/2011gc003678