{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2024,7,24]],"date-time":"2024-07-24T09:17:01Z","timestamp":1721812621807},"reference-count":27,"publisher":"American Association for the Advancement of Science (AAAS)","issue":"5974","content-domain":{"domain":[],"crossmark-restriction":false},"short-container-title":["Science"],"published-print":{"date-parts":[[2010,4,2]]},"abstract":"<jats:title>Sinking Sea Floors<\/jats:title>\n          <jats:p>\n            The depths of ocean bottoms are constantly fluctuating at a very slow rate in response to the generation (at mid-ocean ridges) and consumption (at subduction zones) of sea-floor material. Because older sea floor is susceptible to sinking as it cools, it has been assumed that sea-floor depth varies directly with its age. However,\n            <jats:bold>Adam and Vidal<\/jats:bold>\n            (p.\n            <jats:related-article xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"doi\" page=\"83\" related-article-type=\"in-this-issue\" vol=\"328\" xlink:href=\"10.1126\/science.1185906\">83<\/jats:related-article>\n            ; see the Perspective by\n            <jats:bold>\n              <jats:related-article xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"doi\" issue=\"5974\" page=\"54\" related-article-type=\"in-this-issue\" vol=\"328\" xlink:href=\"10.1126\/science.1188090\">Tolstoy<\/jats:related-article>\n            <\/jats:bold>\n            ) now show that the depth of the Pacific Ocean actually varies in response to the mantle underlying the oceanic crust. This effect is clear when sea-floor depth was measured along lithospheric flow lines\u2014which represent the movement of oceanic crust triggered by mantle convection. Because the ocean bottom does not flatten as predicted by previous models, there is no need to invoke any additional heat supply to sustain old oceanic crust in thermal models of the mantle.\n          <\/jats:p>","DOI":"10.1126\/science.1185906","type":"journal-article","created":{"date-parts":[[2010,4,1]],"date-time":"2010-04-01T20:36:02Z","timestamp":1270154162000},"page":"83-85","source":"Crossref","is-referenced-by-count":23,"title":["Mantle Flow Drives the Subsidence of Oceanic Plates"],"prefix":"10.1126","volume":"328","author":[{"given":"Claudia","family":"Adam","sequence":"first","affiliation":[{"name":"Institute for Research on Earth Evolution, Japan Agency for Marine-Earth Science and Technology, 2-15 Natsushima, Yokosuka, 237-0061, Japan."},{"name":"Centro de Geof\u00edsica, Universidade de \u00c9vora, Rua Rom\u00e3o Ramalho 59, 7002-554 \u00c9vora, Portugal."}]},{"given":"Val\u00e9rie","family":"Vidal","sequence":"additional","affiliation":[{"name":"Laboratoire de Physique, Universit\u00e9 de Lyon, Ecole Normale Sup\u00e9rieure de Lyon\u2013CNRS, 46 All\u00e9e d'Italie, 69364 Lyon cedex 07, France."}]}],"member":"221","reference":[{"key":"e_1_3_2_2_2","doi-asserted-by":"publisher","DOI":"10.1029\/JB080i008p01031"},{"key":"e_1_3_2_3_2","doi-asserted-by":"publisher","DOI":"10.1029\/JB082i005p00803"},{"key":"e_1_3_2_4_2","doi-asserted-by":"publisher","DOI":"10.1038\/359123a0"},{"key":"e_1_3_2_5_2","doi-asserted-by":"publisher","DOI":"10.1016\/0012-821X(96)00082-9"},{"key":"e_1_3_2_6_2","doi-asserted-by":"publisher","DOI":"10.1046\/j.1365-246X.2000.00229.x"},{"key":"e_1_3_2_7_2","doi-asserted-by":"publisher","DOI":"10.1038\/242384a0"},{"key":"e_1_3_2_8_2","doi-asserted-by":"publisher","DOI":"10.1111\/j.1365-246X.2006.03015.x"},{"key":"e_1_3_2_9_2","doi-asserted-by":"publisher","DOI":"10.1029\/JB083iB09p04485"},{"key":"e_1_3_2_10_2","doi-asserted-by":"publisher","DOI":"10.1038\/313125a0"},{"key":"e_1_3_2_11_2","doi-asserted-by":"publisher","DOI":"10.1029\/94GL03297"},{"key":"e_1_3_2_12_2","doi-asserted-by":"publisher","DOI":"10.1029\/2004JB003153"},{"key":"e_1_3_2_13_2","doi-asserted-by":"publisher","DOI":"10.1029\/JB089iB12p09873"},{"key":"e_1_3_2_14_2","doi-asserted-by":"publisher","DOI":"10.1029\/JB093iB09p10467"},{"key":"e_1_3_2_15_2","doi-asserted-by":"publisher","DOI":"10.1086\/629582"},{"key":"e_1_3_2_16_2","doi-asserted-by":"publisher","DOI":"10.1016\/0012-821X(89)90148-9"},{"key":"e_1_3_2_17_2","doi-asserted-by":"publisher","DOI":"10.1016\/0031-9201(90)90109-B"},{"key":"e_1_3_2_18_2","doi-asserted-by":"publisher","DOI":"10.1029\/94JB01747"},{"key":"e_1_3_2_19_2","doi-asserted-by":"publisher","DOI":"10.1016\/S0012-821X(98)00114-9"},{"key":"e_1_3_2_20_2","doi-asserted-by":"publisher","DOI":"10.1029\/2001JB000379"},{"key":"e_1_3_2_21_2","doi-asserted-by":"publisher","DOI":"10.1029\/2004JB002991"},{"key":"e_1_3_2_22_2","doi-asserted-by":"publisher","DOI":"10.1029\/94GL01594"},{"key":"e_1_3_2_23_2","doi-asserted-by":"publisher","DOI":"10.1016\/S0012-821X(99)00218-6"},{"key":"e_1_3_2_25_2","doi-asserted-by":"publisher","DOI":"10.1126\/science.1128489"},{"key":"e_1_3_2_26_2","doi-asserted-by":"publisher","DOI":"10.1046\/j.1365-246X.2002.01627.x"},{"key":"e_1_3_2_27_2","doi-asserted-by":"crossref","unstructured":"T. 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