{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,5,22]],"date-time":"2024-05-22T07:05:50Z","timestamp":1716361550327},"reference-count":32,"publisher":"Wiley","issue":"1","license":[{"start":{"date-parts":[[2014,6,1]],"date-time":"2014-06-01T00:00:00Z","timestamp":1401580800000},"content-version":"vor","delay-in-days":0,"URL":"http:\/\/onlinelibrary.wiley.com\/termsAndConditions#vor"}],"content-domain":{"domain":["onlinelibrary.wiley.com"],"crossmark-restriction":true},"short-container-title":["Near Surface Geophysics"],"published-print":{"date-parts":[[2015,2]]},"abstract":"<jats:title>ABSTRACT<\/jats:title><jats:p>The El Sheikh Zwayed Lake is a saline lake located in northern Sinai Peninsula. The origin of the lake as well as the shallow fresh water supplies between the lake and the Mediterranean are the subject of many geological, hydrogeological, and geophysical studies. Two main hypotheses have been sug gested to explain the phenomenon of the lake (i.e. hydrogeological and\/or tectonic). Using direct current resistivity (DCR) and gravity data, we investigated which of these processes explain the jux taposition and the contradiction between the location of freshwater between the sea and a saline lake to the south which is supplied by a saline aquifer. We infer from the 1D and 2D resistivity inversions that a shallow grabenal structure exists between the lake and the coast. The gravity measurements enable a subsurface NE\u2010SW doubly plunging anticline to be suggested (and related to Syrian arc system) to the south\u2010west side of the lake as well as a NE\u2010SW associated deep inferred fault\u2010line crossing the lake. The results show that the hydrogeological regime in the study area is tectonically con trolled; whereby the graben structure works as a hydrogeological barrier between the lake and the sea.<\/jats:p>","DOI":"10.3997\/1873-0604.2014047","type":"journal-article","created":{"date-parts":[[2015,1,15]],"date-time":"2015-01-15T10:02:40Z","timestamp":1421316160000},"page":"93-101","update-policy":"http:\/\/dx.doi.org\/10.1002\/crossmark_policy","source":"Crossref","is-referenced-by-count":2,"title":["Geophysical evidence for the hydro\u2010tectonic origin of the Sabkha El Sheikh Zwayed Lake and the shallow fresh water supplies, Northern Sinai, Egypt"],"prefix":"10.1002","volume":"13","author":[{"given":"Mohamed A.","family":"Khalil","sequence":"first","affiliation":[{"name":"Universidade de Lisboa\u2010IDL Campo Grande, Ed. C8  1749\u2010016 Lisbon Portugal"},{"name":"National Research Institute of Astronomy and Geophysics (NRIAG)  Helwan, Cairo Egypt"}]},{"given":"Fernando M.","family":"Santos","sequence":"additional","affiliation":[{"name":"Universidade de Lisboa\u2010IDL Campo Grande, Ed. C8  1749\u2010016 Lisbon Portugal"}]}],"member":"311","published-online":{"date-parts":[[2014,6]]},"reference":[{"key":"e_1_2_5_1_2_1","volume-title":"Moscow State University","author":"Bobachev A.A.","year":"2000"},{"key":"e_1_2_5_1_3_1","doi-asserted-by":"publisher","DOI":"10.1090\/S0025-5718-1965-0198670-6"},{"key":"e_1_2_5_1_4_1","doi-asserted-by":"publisher","DOI":"10.1190\/1.1444729"},{"key":"e_1_2_5_1_5_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0098-3004(01)00039-5"},{"key":"e_1_2_5_1_6_1","doi-asserted-by":"publisher","DOI":"10.1016\/0040-1951(87)90184-3"},{"key":"e_1_2_5_1_7_1","volume-title":"Vol. II\u2010A and II\u2010B: Report submitted to the Advisory Committee for Reconstruction","author":"Dames","year":"1984"},{"key":"e_1_2_5_1_8_1","first-page":"1386","article-title":"Miocene sandstone provenance relations in the Gulf of Suez: insights into sy\u2010nrift unroofing and uplift history. 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