{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,1,19]],"date-time":"2026-01-19T02:16:48Z","timestamp":1768789008988,"version":"3.49.0"},"reference-count":78,"publisher":"Geological Society of London","issue":"2","license":[{"start":{"date-parts":[[2009,2,27]],"date-time":"2009-02-27T00:00:00Z","timestamp":1235692800000},"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":[[2009,3]]},"abstract":"<jats:title>Abstract:<\/jats:title>\n          <jats:p>\n            Mantle peridotitic xenoliths in Cenozoic basalts from Hannuoba, on the northern margin of the Archaean North China Craton, have variable Re (0.01\u20130.30 ppb) and Os (2.7\u20136.2 ppb) abundances and\n            <jats:sup>187<\/jats:sup>\n            Os\/\n            <jats:sup>188<\/jats:sup>\n            Os (0.1138\u20130.1236) ratios. These xenoliths yield a range of Proterozoic Re depletion ages of 0.8\u20132.2 Ga that show a general correlation with olivine Fo. Mantle xenoliths in Cenozoic basalts from the centre and southern margin of the North China Craton also overwhelmingly show Proterozoic Re depletion ages that correlate with olivine Fo. These Re\u2013Os age features are completely different from those of Palaeozoic kimberlite-borne peridotitic xenoliths, which have Archaean ages. This age distinction between xenoliths associated with Palaeozoic and Cenozoic volcanism indicates that the present-day lithospheric mantle was dominantly not newly accreted during the Phanerozoic but instead was transformed from the ancient lithospheric mantle by interaction with melts. The Re\u2013Os data in combination with the geochemical and Sr\u2013Nd isotopic features of peridotitic xenoliths from the Cenozoic basalts of the North China Craton demonstrate the presence of multiple stages of mantle metasomatic overprints in the lithospheric mantle. This study thus further indicates that lithospheric transformation through melt\u2013rock interaction could be an important mechanism for compositional refertilization during the Phanerozoic.\n          <\/jats:p>\n          <jats:sec>\n            <jats:title>Supplementary material:<\/jats:title>\n            <jats:p>\n              Analytical methods and geochemical data are available at\n              <jats:uri xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" xlink:href=\"http:\/\/www.geolsoc.org.uk\/SUP18334\" xlink:type=\"simple\">http:\/\/www.geolsoc.org.uk\/SUP18334<\/jats:uri>\n              .\n            <\/jats:p>\n          <\/jats:sec>","DOI":"10.1144\/0016-76492007-152","type":"journal-article","created":{"date-parts":[[2009,2,28]],"date-time":"2009-02-28T03:00:45Z","timestamp":1235790045000},"page":"249-259","source":"Crossref","is-referenced-by-count":107,"title":["Comprehensive refertilization of lithospheric mantle beneath the North China Craton: further Os\u2013Sr\u2013Nd isotopic constraints"],"prefix":"10.1144","volume":"166","author":[{"given":"Hong-Fu","family":"Zhang","sequence":"first","affiliation":[{"name":"State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences,PO Box 9825, Beijing 100029, China"}]},{"given":"Steven L.","family":"Goldstein","sequence":"additional","affiliation":[{"name":"Lamont\u2013Doherty Earth Observatory and Department of Earth and Environmental Sciences, Columbia University,61 Rt. 9W, Palisades, NY 10964, USA"}]},{"given":"Xin-Hua","family":"Zhou","sequence":"additional","affiliation":[{"name":"State Key Laboratory of Lithospheric Evolution, Institute of Geology and Geophysics, Chinese Academy of Sciences,PO Box 9825, Beijing 100029, China"}]},{"given":"Min","family":"Sun","sequence":"additional","affiliation":[{"name":"Department of Earth Sciences, University of Hong Kong, Pokfulam Road, Hong Kong, China"}]},{"given":"Yue","family":"Cai","sequence":"additional","affiliation":[{"name":"Lamont\u2013Doherty Earth Observatory and Department of Earth and Environmental Sciences, Columbia University,61 Rt. 9W, Palisades, NY 10964, USA"}]}],"member":"1881","published-online":{"date-parts":[[2009,2,27]]},"reference":[{"key":"e_1_3_2_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/0016-7037(89)90286-X"},{"key":"e_1_3_2_3_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0012-821X(01)00308-9"},{"key":"e_1_3_2_4_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0012-821X(97)00167-2"},{"key":"e_1_3_2_5_1","doi-asserted-by":"publisher","DOI":"10.1093\/petrology\/31.3.597"},{"key":"e_1_3_2_6_1","doi-asserted-by":"publisher","DOI":"10.1016\/0012-821X(89)90120-9"},{"key":"e_1_3_2_7_1","doi-asserted-by":"publisher","DOI":"10.1038\/315387a0"},{"key":"e_1_3_2_8_1","doi-asserted-by":"publisher","DOI":"10.1126\/science.272.5263.861"},{"key":"e_1_3_2_9_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0012-821X(00)00044-3"},{"key":"e_1_3_2_10_1","doi-asserted-by":"publisher","DOI":"10.1016\/0012-821X(94)90124-4"},{"key":"e_1_3_2_11_1","doi-asserted-by":"publisher","DOI":"10.1029\/2005JB003974"},{"key":"e_1_3_2_12_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0024-4937(00)00065-7"},{"key":"e_1_3_2_13_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0016-7037(99)00004-6"},{"key":"e_1_3_2_14_1","first-page":"106","volume-title":"Diamonds: Characterization, Genesis and Exploration. 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