{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2025,2,21]],"date-time":"2025-02-21T12:52:48Z","timestamp":1740142368618,"version":"3.37.3"},"reference-count":27,"publisher":"Geological Society of London","issue":"3","license":[{"start":{"date-parts":[[2019,6,9]],"date-time":"2019-06-09T00:00:00Z","timestamp":1560038400000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"funder":[{"DOI":"10.13039\/501100001691","name":"Japan Society for the Promotion of Science","doi-asserted-by":"crossref","award":["20340139"],"award-info":[{"award-number":["20340139"]}],"id":[{"id":"10.13039\/501100001691","id-type":"DOI","asserted-by":"crossref"}]}],"content-domain":{"domain":["www.lyellcollection.org"],"crossmark-restriction":true},"short-container-title":["JGS"],"published-print":{"date-parts":[[2020,5]]},"abstract":"<jats:p>The progressive development of microfabrics from initial deposition to slump deformation and then a submarine slide was investigated in an active subduction zone using cores recovered during the Integrated Ocean Drilling Program Expedition 333. A Pleistocene\u2013Holocene sequence was recovered at Site C0018A, which was located on a slope basin on the footwall of the megasplay fault in the Nankai Trough, SW Japan. Six mass-transport deposit units intercalated with coherent intervals were recovered from the upper 190\u2005m of the drilled succession. The initial microfabrics in the undeformed hemipelagic sediments were characterized by random and porous fabrics composed predominantly of clay aggregations and connectors. The initial fabrics were cardhouse fabrics, which consist of clay flakes with edge-to-edge (E\u2013E) and\/or edge-to-face (E\u2013F) contacts. These initial microfabrics developed into compacted microfabrics, which are random and consolidated fabrics (bookhouse fabrics) that consist of clay flakes with E\u2013F and\/or face-to-face (F\u2013F) contacts and develop during burial as a pure shear deformation. During slumping, these fabrics were then deformed under simple shear to become predominantly F\u2013F contacts and form clay chains. Thus, the microfabrics in these submarine slides are a sedimentary m\u00e9lange that developed locally into a preferred clay orientation with F\u2013F contacts.<\/jats:p>\n          <jats:p content-type=\"supplementary-material\">\n            <jats:bold>Supplementary material:<\/jats:bold>\n            A schematic illustration showing sedimentation processes and fabrics is available at\n            <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" specific-use=\"dataset is-supplemented-by\" xlink:href=\"https:\/\/doi.org\/10.6084\/m9.figshare.c.4483385\">https:\/\/doi.org\/10.6084\/m9.figshare.c.4483385<\/jats:ext-link>\n          <\/jats:p>\n          <jats:p content-type=\"thematic-collection\">\n            <jats:bold>Thematic collection:<\/jats:bold>\n            This article is part of the Polygenetic m\u00e9langes collection available at:\n            <jats:ext-link xmlns:xlink=\"http:\/\/www.w3.org\/1999\/xlink\" ext-link-type=\"uri\" xlink:href=\"https:\/\/www.lyellcollection.org\/cc\/polygenetic-melanges\">https:\/\/www.lyellcollection.org\/cc\/polygenetic-melanges<\/jats:ext-link>\n          <\/jats:p>","DOI":"10.1144\/jgs2018-218","type":"journal-article","created":{"date-parts":[[2019,4,30]],"date-time":"2019-04-30T16:11:12Z","timestamp":1556640672000},"page":"619-628","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":2,"title":["The progressive development of microfabrics from initial deposition to slump deformation: an example from a modern sedimenary m\u00e9lange on the Nankai Prism"],"prefix":"10.1144","volume":"177","author":[{"given":"Mebae","family":"Kuranaga","sequence":"first","affiliation":[{"name":"Graduate School of Science and Technology for Innovation, Yamaguchi University, 1677-1 Yoshida, Yamaguchi-city, Yamaguchi 753-8512, Japan"},{"name":"Taiheiyo Consultant Co. Ltd, 2-2-4 Daisaku, Sakura-city, Chiba 285-0802, Japan"}]},{"ORCID":"https:\/\/orcid.org\/0000-0003-0501-4033","authenticated-orcid":false,"given":"Kiichiro","family":"Kawamura","sequence":"additional","affiliation":[{"name":"Graduate School of Science and Technology for Innovation, Yamaguchi University, 1677-1 Yoshida, Yamaguchi-city, Yamaguchi 753-8512, Japan"}]},{"ORCID":"https:\/\/orcid.org\/0000-0002-7108-4534","authenticated-orcid":false,"given":"Toshiya","family":"Kanamatsu","sequence":"additional","affiliation":[{"name":"Japan Agency for Marine Science and Technology, 2-15 Natsushima, Yokosuka, Kanagawa 237-0046, Japan"}]}],"member":"1881","published-online":{"date-parts":[[2019,6,9]]},"reference":[{"key":"e_1_3_3_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/0040-1951(75)90102-X"},{"key":"e_1_3_3_3_1","first-page":"217","article-title":"Clay fabric of selected submarine sediments: fundamental properties and models","volume":"51","author":"Bennett R.H.","year":"1981","unstructured":"Bennett, R.H., Bryant, W.R. & Keller, G.H. 1981. Clay fabric of selected submarine sediments: fundamental properties and models. Journal of Sedimentary Petrology, 51, 217\u2013232, https:\/\/doi.org\/10.1306\/212F7C52-2B24-11D7-8648000102C1865D","journal-title":"Journal of Sedimentary Petrology"},{"key":"e_1_3_3_4_1","doi-asserted-by":"publisher","DOI":"10.2973\/odp.tn.26.1997"},{"key":"e_1_3_3_5_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.tecto.2012.08.002"},{"key":"e_1_3_3_6_1","doi-asserted-by":"crossref","unstructured":"Expedition 333 Scientists 2012. Site C0018. In : Henry P. Kanamatsu T. 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