{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,6,2]],"date-time":"2026-06-02T23:46:32Z","timestamp":1780443992002,"version":"3.54.1"},"reference-count":41,"publisher":"Society for Sedimentary Geology","issue":"8","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":[],"published-print":{"date-parts":[[2013,8,1]]},"abstract":"<jats:title>Abstract:\u2003<\/jats:title>\n                  <jats:p>Whole-rock, inorganic, geochemical data have previously been used to aid characterization and stratigraphic correlation of fossil-poor clastic sedimentary deposits, although this approach has not yet been calibrated by testing chemostratigraphic correlations against physical stratigraphic correlations from outcrop. Chemical data from a well-exposed siliciclastic succession in a Tortonian (late Miocene) submarine slope channel system in the Tabernas Basin of southern Spain were generated using X-ray fluorescence supplemented by X-ray diffraction, SEM analysis, and light microscopy. Amongst the &amp;gt;\u200960 elements measured, nearly a quarter of them have proved to be useful or reliable for geochemically based correlation at the tested scales (\u223c\u200910\u00a0m, \u223c\u200950\u00a0m, \u223c\u2009100\u00a0m). These elements are SiO2, K2O, Al2O3, CaO, and TiO2, as well as Zr, Nb, Th, Rb, Cs, As, and the rare earth elements, La, Nd, and Ce. High-resolution, bed-to-bed geochemical correlation is feasible over short distances (\u223c\u200910\u00a0m). Geochemical data from sections in beds that are traceable suggest that a given stratigraphic level seems to be geochemically homogeneous with respect to some key elements. Geochemical data also provide a useful aid for high-resolution sedimentary correlation, at distances of several tens of meters up to at least 100\u00a0m. Since each individual bed seems to be broadly homogeneous in composition, at a larger scale it is possible to discern a provenance signal in geochemical data. Chemical stratigraphy thus seems to work even in stratigraphically complicated submarine channel complexes.<\/jats:p>","DOI":"10.2110\/jsr.2013.41","type":"journal-article","created":{"date-parts":[[2013,7,31]],"date-time":"2013-07-31T03:37:12Z","timestamp":1375241832000},"page":"669-690","source":"Crossref","is-referenced-by-count":7,"title":["Geochemical Correlation In An Exhumed Submarine Channel Complex (Tabernas Basin, Se Spain): Comparison To Sedimentological Correlation At Various Length Scales"],"prefix":"10.2110","volume":"83","author":[{"given":"Michaela","family":"Aehnelt","sequence":"first","affiliation":[{"name":"1\u2009Department of Earth and Ocean Sciences, School of Environmental Sciences, University of Liverpool, 4 Brownlow Street, Liverpool L69 3GP, U.K."},{"name":"2\u2009IReS Ltd., The Technology Centre, Inward Way Rossmore Business Park, Ellesmere Port CH65 3EN, U.K."}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Richard H.","family":"Worden","sequence":"additional","affiliation":[{"name":"1\u2009Department of Earth and Ocean Sciences, School of Environmental Sciences, University of Liverpool, 4 Brownlow Street, Liverpool L69 3GP, U.K."}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Andrew C.","family":"Canham","sequence":"additional","affiliation":[{"name":"2\u2009IReS Ltd., The Technology Centre, Inward Way Rossmore Business Park, Ellesmere Port CH65 3EN, U.K."}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Stephen J.","family":"Hill","sequence":"additional","affiliation":[{"name":"2\u2009IReS Ltd., The Technology Centre, Inward Way Rossmore Business Park, Ellesmere Port CH65 3EN, U.K."}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"David M.","family":"Hodgson","sequence":"additional","affiliation":[{"name":"1\u2009Department of Earth and Ocean Sciences, School of Environmental Sciences, University of Liverpool, 4 Brownlow Street, Liverpool L69 3GP, U.K."}],"role":[{"vocabulary":"crossref","role":"author"}]},{"given":"Stephen S.","family":"Flint","sequence":"additional","affiliation":[{"name":"1\u2009Department of Earth and Ocean Sciences, School of Environmental Sciences, University of Liverpool, 4 Brownlow Street, Liverpool L69 3GP, U.K."}],"role":[{"vocabulary":"crossref","role":"author"}]}],"member":"860","published-online":{"date-parts":[[2013,8,1]]},"reference":[{"key":"2026060205230591100_i1527-1404-83-8-669-Abreu1","doi-asserted-by":"crossref","first-page":"631","DOI":"10.1016\/j.marpetgeo.2003.08.003","article-title":"Lateral accretion packages (LAPs): an important reservoir element in deep water sinuous channels","volume":"20","author":"Abreu","year":"2003","journal-title":"Marine and Petroleum Geology"},{"key":"2026060205230591100_i1527-1404-83-8-669-Andersson1","first-page":"21, p. 555\u2013577","volume-title":"Provenance evolution and chemostratigraphy of a Palaeozoic submarine fan-complex: Tanqua Karoo Basin, South 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