{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,10,3]],"date-time":"2025-10-03T17:55:16Z","timestamp":1759514116189},"reference-count":27,"publisher":"Geological Society of London","issue":"1","license":[{"start":{"date-parts":[[2013,1,1]],"date-time":"2013-01-01T00:00:00Z","timestamp":1356998400000},"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":["SP"],"published-print":{"date-parts":[[2013,1]]},"abstract":"<jats:title>Abstract<\/jats:title>\n          <jats:p>\n            We have studied the rock magnetic and palaeomagnetic properties of a 41 m long core (Hole M0058A) recovering calcareous sediments located seaward of Noggin Reef, offshore Queensland, Australia to decipher the magnetostratigrapy of the site. We deployed 1 cm\n            <jats:sup>3<\/jats:sup>\n            samples at every 10 cm down-core and subsampled the core by means of U-channels in order to obtain a continuous record. Stepwise alternating field demagnetization from natural remanent magnetization to 80 mT showed that the characteristic remanent magnetization was isolated at low demagnetization fields between 0 and 15 mT. We conducted magnetic granulometry analyses and Curie point determinations. The low-field v. temperature analyses indicate the presence of Ti-poor magnetite with Curie points from 560 to 563 \u00b0C. Hysteresis loop experiments were performed. The results show\n            <jats:italic>M<\/jats:italic>\n            <jats:sub>rs<\/jats:sub>\n            \/\n            <jats:italic>M<\/jats:italic>\n            <jats:sub>s<\/jats:sub>\n            and\n            <jats:italic>H<\/jats:italic>\n            <jats:sub>cr<\/jats:sub>\n            \/\n            <jats:italic>H<\/jats:italic>\n            <jats:sub>c<\/jats:sub>\n            ratios corresponding to single domain to multi-domain and super-paramagnetic to single domain ranges. Both discrete and continuous inclination results indicate a remarkable correlation of three excursional inclinations occurring during intervals of low intensity of magnetization closely corresponding to the Laschamp (\n            <jats:italic>c.<\/jats:italic>\n            41 ka), Sk\u00e1lam\u00e6lifell (\n            <jats:italic>c.<\/jats:italic>\n            94 ka) and Blake (\n            <jats:italic>c.<\/jats:italic>\n            115\u2013120 ka) \u2018aborted reversals,\u2019 and indicate that the base of the core is much older than the Blake excursion.\n          <\/jats:p>","DOI":"10.1144\/sp373.19","type":"journal-article","created":{"date-parts":[[2013,4,26]],"date-time":"2013-04-26T04:01:47Z","timestamp":1366948907000},"page":"279-291","source":"Crossref","is-referenced-by-count":1,"title":["On the palaeomagnetic and rock magnetic constraints regarding the age of IODP 325 Hole M0058A"],"prefix":"10.1144","volume":"373","author":[{"given":"Emilio","family":"Herrero-Bervera","sequence":"first","affiliation":[{"name":"Hawaii Institute of Geophysics and Planetology, University of Hawaii, Honolulu, HI 96822, USA"}],"role":[{"role":"author","vocabulary":"crossref"}]},{"given":"Luigi","family":"Jovane","sequence":"additional","affiliation":[{"name":"Department of Geology, Western Washington University, Bellingham, WA 98225, USA"},{"name":"Instituto Ocenogr\u00e1fico, Universidade de S\u00e3o Paulo, S\u00e3o Paulo 05508-120, Brazil"}],"role":[{"role":"author","vocabulary":"crossref"}]}],"member":"1881","published-online":{"date-parts":[[2013,4,25]]},"reference":[{"key":"e_1_3_2_2_1","doi-asserted-by":"publisher","DOI":"10.2973\/odp.proc.sr.133.261.1993"},{"key":"e_1_3_2_3_1","doi-asserted-by":"publisher","DOI":"10.2973\/odp.proc.sr.133.285.1993"},{"key":"e_1_3_2_4_1","doi-asserted-by":"publisher","DOI":"10.1038\/scientificamerican1281-58"},{"key":"e_1_3_2_5_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.epsl.2006.01.021"},{"key":"e_1_3_2_6_1","doi-asserted-by":"publisher","DOI":"10.1029\/2001JB000487"},{"key":"e_1_3_2_7_1","doi-asserted-by":"publisher","DOI":"10.2204\/iodp.proc.325.106.2011"},{"key":"e_1_3_2_8_1","doi-asserted-by":"publisher","DOI":"10.1038\/20420"},{"key":"e_1_3_2_9_1","doi-asserted-by":"publisher","DOI":"10.1029\/2002GL014963."},{"key":"e_1_3_2_10_1","doi-asserted-by":"publisher","DOI":"10.1111\/j.1365-246X.1992.tb04634.x"},{"key":"e_1_3_2_11_1","doi-asserted-by":"publisher","DOI":"10.1098\/rsta.1997.0089"},{"key":"e_1_3_2_12_1","doi-asserted-by":"publisher","DOI":"10.1016\/0031-9201(87)90034-3"},{"key":"e_1_3_2_13_1","doi-asserted-by":"publisher","DOI":"10.1111\/j.1365-246X.1994.tb03987.x"},{"key":"e_1_3_2_14_1","doi-asserted-by":"publisher","DOI":"10.1111\/j.1365-246X.1997.tb04506.x"},{"key":"e_1_3_2_15_1","doi-asserted-by":"publisher","DOI":"10.5636\/jgg.36.45"},{"key":"e_1_3_2_16_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.epsl.2011.08.007"},{"key":"e_1_3_2_17_1","doi-asserted-by":"publisher","DOI":"10.1111\/1758-2229.12000"},{"key":"e_1_3_2_18_1","doi-asserted-by":"publisher","DOI":"10.1029\/GM128p0051"},{"key":"e_1_3_2_19_1","doi-asserted-by":"publisher","DOI":"10.1111\/j.1365-246X.1980.tb02601.x"},{"key":"e_1_3_2_20_1","doi-asserted-by":"publisher","DOI":"10.1017\/CBO9780511535635"},{"key":"e_1_3_2_21_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.epsl.2010.03.002"},{"key":"e_1_3_2_22_1","doi-asserted-by":"publisher","DOI":"10.1029\/95JB02811"},{"key":"e_1_3_2_23_1","doi-asserted-by":"publisher","DOI":"10.1007\/978-1-4020-4423-6_266"},{"key":"e_1_3_2_24_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0012-821X(03)00701-5"},{"key":"e_1_3_2_25_1","doi-asserted-by":"publisher","DOI":"10.1038\/366234a0"},{"key":"e_1_3_2_26_1","doi-asserted-by":"publisher","DOI":"10.1038\/nature03674"},{"key":"e_1_3_2_27_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.epsl.2008.07.056"},{"key":"e_1_3_2_28_1","doi-asserted-by":"publisher","DOI":"10.1016\/0012-821X(91)90122-X"}],"container-title":["Geological 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