Zobrazeno 1 - 10
of 28
pro vyhledávání: '"Avihu Ginzburg"'
Publikováno v:
Israel Journal of Earth Sciences. 55:129-139
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::c2cb29954bae2bc4744031cdbb7cbcf6
https://doi.org/10.1560/ijes_55_3_129
https://doi.org/10.1560/ijes_55_3_129
Publikováno v:
Tectonophysics. 346:23-43
A seismic refraction/wide-angle reflection experiment was undertaken in the Levant Basin, eastern Mediterranean. Two roughly east–west profiles extend from the continental shelf of Israel toward the Levant Basin. The northern profile crosses the Er
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::d73f90d166e2c5be6695f242c61c5b25
https://doi.org/10.1016/s0040-1951(01)00226-8
https://doi.org/10.1016/s0040-1951(01)00226-8
Publikováno v:
Geophysical Journal International. 134:460-472
The present study utilizes the Israel Seismic Network (ISN) as a spatially distributed multichannel system for the discrimination of low-magnitude events (ML
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::941cbb9917dfb7106015b04e74a770bd
https://doi.org/10.1046/j.1365-246x.1998.00566.x
https://doi.org/10.1046/j.1365-246x.1998.00566.x
Autor:
Avihu Ginzburg, Zvi Ben-Avraham
Publikováno v:
Geophysical Research Letters. 24:2063-2066
A seismic refraction experiment involving the use of 9 OBS and 11 portable seismic land stations was conducted along a profile in the north basin of the Dead Sea. The seismometers were deployed along a north-south profile in the lake and the adjacent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4836efb3585df6669f611ffcd9390581
https://doi.org/10.1029/97gl01884
https://doi.org/10.1029/97gl01884
Autor:
Avihu Ginzburg, Michael Lazar, Zvi Ben-Avraham, Moshe Reshef, Y. Bartov, U. Frieslander, Zvi Garfunkel, Haim Shulman, Y. Rotstein
The Dead Sea fault is a left-lateral transform plate boundary separating the Arabian Plate and the Sinai sub-plate. Motion along the fault is not pure strike-slip and the direction of the plate boundary changes several times resulting in areas of tra
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::500d71094e022763a336943b39fcd4e9
https://doi.org/10.1016/b978-0-444-56357-6.00016-0
https://doi.org/10.1016/b978-0-444-56357-6.00016-0
Autor:
Avihu Ginzburg, Zvi Ben-Avraham
Publikováno v:
Tectonics. 9:613-622
Geophysical data from the Levant and the eastern Mediterranean suggest that this area can be divided into distinct crustal units of different origins. For example, a marked difference in crustal structure and structural style exists in the Levant bet
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::9df57ab5ed0d9253d8bf5bcbe598a1c5
https://doi.org/10.1029/tc009i004p00613
https://doi.org/10.1029/tc009i004p00613
Autor:
Avihu Ginzburg, Amos Levanon
Publikováno v:
Geoexploration. 15:47-56
Direct current resistivity surveys, using modified exploration techniques, were conducted at two archaeological sites in Israel. In the area of the Temple of the Mount in Jerusalem the thickness of the south wall and Wailing Wall was accurately deter
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::ebf17a79c2a72117d53caa6d2e22bc55
https://doi.org/10.1016/0016-7142(77)90006-0
https://doi.org/10.1016/0016-7142(77)90006-0
Publikováno v:
Tectonophysics. 80:121-133
The recent acquisition of high-quality seismic refraction data in the Jordan—Dead Sea rift and adjacent areas has made possible the investigation of the dynamic properties of seismic P-waves refracted and reflected at the crust—upper mantle bound
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::813bd21c49ce77e882afe427851793c4
https://doi.org/10.1016/0040-1951(81)90145-1
https://doi.org/10.1016/0040-1951(81)90145-1
Publikováno v:
Tectonophysics. 80:109-119
The previously published results of a deep seismic refraction study of the Dead Sea—Gulf of Elat rift show crustal thinning underneath the rift and the presence of a 5 km thick velocity transition zone in the lower crust along the rift. The structu
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::698df1bf4d56b4ecc57438970ff3b80a
https://doi.org/10.1016/0040-1951(81)90144-x
https://doi.org/10.1016/0040-1951(81)90144-x