{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,3,26]],"date-time":"2026-03-26T22:59:31Z","timestamp":1774565971813,"version":"3.50.1"},"reference-count":74,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[2013,10,23]],"date-time":"2013-10-23T00:00:00Z","timestamp":1382486400000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["JGS"],"published-print":{"date-parts":[[2014,1]]},"abstract":"<jats:p>The Nile drains a large basin covering various source-rock terrains of different age, mineralogical and isotopic characteristics. Its sediments are stored within the Nile delta but significant volumes are swept eastwards in the SE Mediterranean, onto the Sinai\u2013Israeli coasts. Alongside wave transport, aeolian transport plays an important role in recycling the Nile-derived sands. We present new laser ablation inductively coupled plasma mass spectrometry, 882 U\u2013Pb and 586 Lu\u2013Hf analyses of detrital zircons from Quaternary to Recent sands of the Israeli coast and shelf to decipher their provenance. The detrital populations are dominated by 0.56\u20131.15 Ga zircons with \u03f5Hf(t) of +13 to \u221227, implying a mixture of juvenile and non-juvenile latest Mesoproterozoic to Neoproterozoic sources. Small populations of Archaean\u2013Palaeoproterozoic and Palaeozoic zircons are also distinguished. The detrital zircon U\u2013Pb\u2013Hf pattern indicates that rather than being sourced from the Arabian\u2013Nubian Shield or older basement terranes in the Nile drainage basin, the sands are dominantly recycling products of older sediments. The detrital zircon U\u2013Pb\u2013Hf spectra resemble those of Cambro-Ordovician sandstones that blanket much of North Africa. These sediments were recycled into younger sand reservoirs that were in turn eroded into the Nile and transported to the coast of Israel.<\/jats:p>\n          <jats:sec>\n            <jats:title>Supplementary material:<\/jats:title>\n            <jats:p>\n              Details of analytical methods and detrital zircon U\u2013Pb\u2013Hf data are available at\n              <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" xlink:href=\"http:\/\/www.geolsoc.org.uk\/SUP18677\">www.geolsoc.org.uk\/SUP18677<\/jats:ext-link>\n              .\n            <\/jats:p>\n          <\/jats:sec>","DOI":"10.1144\/jgs2012-151","type":"journal-article","created":{"date-parts":[[2013,10,24]],"date-time":"2013-10-24T01:30:50Z","timestamp":1382578250000},"page":"107-116","source":"Crossref","is-referenced-by-count":32,"title":["Detrital zircon U\u2013Pb\u2013Hf systematics of Israeli coastal sands: new perspectives on the provenance of Nile sediments"],"prefix":"10.1144","volume":"171","author":[{"given":"Y.","family":"Be\u2019eri-Shlevin","sequence":"first","affiliation":[{"name":"Institute of Earth Sciences, Hebrew University, Edmond J. 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