Zobrazeno 1 - 10
of 76
pro vyhledávání: '"M. Beyth"'
Publikováno v:
International Journal of Earth Sciences. 107:1431-1443
The sinistral displacement along the Dead Sea Transform (DST), the plate boundary between the African and the Arabian plates, south of the Dead Sea basin, was previously attributed to two main fault zones: the Arava/Araba or Dead Sea fault and the Fe
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::48e657f49e3be72097787e63d9076576
https://doi.org/10.1007/s00531-017-1549-7
https://doi.org/10.1007/s00531-017-1549-7
Publikováno v:
Journal of African Earth Sciences. 99:332-341
Recently, a detailed (1:50,000) geological map of the Elat area, southern Israel was published. Attached to this map is a stratigraphic table of the Neoproterozoic metamorphic–magmatic complex of the study area. The Neoproterozoic basement in the E
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::95645767181cf2808030609a838daf5d
https://doi.org/10.1016/j.jafrearsci.2014.03.028
https://doi.org/10.1016/j.jafrearsci.2014.03.028
Autor:
M. Beyth, Zvi Garfunkel
Publikováno v:
Geological Society, London, Special Publications. 259:23-42
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5bb779fb9ab2946310da54291867941a
https://doi.org/10.1144/gsl.sp.2006.259.01.04
https://doi.org/10.1144/gsl.sp.2006.259.01.04
Autor:
R. Hofstetter, M. Beyth
Publikováno v:
Geophysical Journal International. 155:715-732
SUMMARY We studied the seismic activity of the Afar Depression (AD) and adjacent regions during the period 1960‐2000. We define seven distinct seismogenic regions using geological, tectonic and seismological data. Based on the frequency‐magnitude
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::295fe4c3f66d6bc6100f461b49ff27db
https://doi.org/10.1046/j.1365-246x.2003.02080.x
https://doi.org/10.1046/j.1365-246x.2003.02080.x
Publikováno v:
Journal of Geochemical Exploration. 46:349-364
In terms of geochemical sampling and evaluation, arid zones may be broadly classified into two categories: mountainous, where areas of rock exposures dominate over those covered by alluvium, and relatively flat areas, where alluvium (and sand) domina
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::43a9b1ab4b6589bcc76c807808ec1d92
https://doi.org/10.1016/0375-6742(93)90030-p
https://doi.org/10.1016/0375-6742(93)90030-p
Autor:
M. Beyth, M. Goldberg
Publikováno v:
Tectonophysics. 198:261-273
Tiran Island and the Strait of Tiran are part of a compressional segment at the southern end of the Dead Sea transform. During the Late Oligocene and Miocene, the area was controlled by tensional tectonics; at that time the Tiran and Shadwan islands
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::f576c93e7c507973e33028b76a34bef2
https://doi.org/10.1016/0040-1951(91)90154-k
https://doi.org/10.1016/0040-1951(91)90154-k
Publikováno v:
Israel Geological Society Annual Meeting, Eilat
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=dedup_wf_001::4b0dedac773b7298e32c4d719afa20a2
https://gfzpublic.gfz-potsdam.de/pubman/item/item_228582
https://gfzpublic.gfz-potsdam.de/pubman/item/item_228582
Publikováno v:
Proc. IGARSS´97
The ERS-1/2 tandem mission opened a new dimension in the detection of recent displacements of active tectonic structures like the Dead Sea Rift in Israel. The investigations are mainly concentrated on the northern coastal plains of the Gulf of Aqaba
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::d0461f32d4e3766375c988bd82b0c605
https://gfzpublic.gfz-potsdam.de/pubman/item/item_227249
https://gfzpublic.gfz-potsdam.de/pubman/item/item_227249
Akademický článek
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Autor:
M. Beyth, Ron Goldbery
Publikováno v:
Sedimentology. 31:575-594
Field and laboratory investigations of the Triassic Budra Formation of Wadi Budra, south-west Sinai, have demonstrated the existence of surface pedogenic laterites developed within‘overbank facies’of fluviatile sediments during times of hiatus. T
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::58ebe085e7c586db23ff398a867433bb
https://doi.org/10.1111/j.1365-3091.1984.tb01821.x
https://doi.org/10.1111/j.1365-3091.1984.tb01821.x