{"status":"ok","message-type":"work","message-version":"1.0.0","message":{"indexed":{"date-parts":[[2026,2,27]],"date-time":"2026-02-27T03:45:53Z","timestamp":1772163953851,"version":"3.50.1"},"reference-count":59,"publisher":"Geological Society of London","issue":"2","license":[{"start":{"date-parts":[[2017,11,1]],"date-time":"2017-11-01T00:00:00Z","timestamp":1509494400000},"content-version":"stm-asf","delay-in-days":0,"URL":"https:\/\/doi.org\/10.15223\/policy-002"}],"funder":[{"name":"Horizon 2020","award":["642976"],"award-info":[{"award-number":["642976"]}]}],"content-domain":{"domain":["www.lyellcollection.org"],"crossmark-restriction":true},"short-container-title":["JGS"],"published-print":{"date-parts":[[2018,3]]},"abstract":"<jats:p>\n                    Tillite lithified by magnesium silicate hydrate (M-S-H) cement has been formed at the surface of the Feragen Ultramafic Body in SE Norway. Serpentinization of olivine-rich rocks led to formation of brucite, which dissolves during weathering to form a high-pH (&gt;9) Mg-rich fluid. This fluid dissolves quartz deposited by glaciers during the Weichselian glaciation. Subsequent evaporation leads to the precipitation of a nanocrystalline magnesium silicate hydrate phase with the approximate composition Mg\n                    <jats:sub>8<\/jats:sub>\n                    Si\n                    <jats:sub>8<\/jats:sub>\n                    O\n                    <jats:sub>20<\/jats:sub>\n                    (OH)\n                    <jats:sub>8<\/jats:sub>\n                    \u00b76H\n                    <jats:sub>2<\/jats:sub>\n                    O. The resulting cemented rock is characterized by disintegrated and partly dissolved quartz grains that are surrounded by the M-S-H cement. This process occurs at surface conditions in a subarctic climate and is known to take place on a timescale of a few decades, as constrained by mining activities. Magnesium-based cement is currently of high interest as the search for environmentally friendly cement is a pressing task considering that the widely used Portland cement accounts for about 7% of the worldwide anthropogenic CO\n                    <jats:sub>2<\/jats:sub>\n                    emission. As this study provides new key insights into the formation process of natural CO\n                    <jats:sub>2<\/jats:sub>\n                    -neutral magnesium-based cement on the field- and microscale, it could contribute in the development of a new sustainable construction material.\n                  <\/jats:p>","DOI":"10.1144\/jgs2017-089","type":"journal-article","created":{"date-parts":[[2017,11,1]],"date-time":"2017-11-01T20:20:16Z","timestamp":1509567616000},"page":"308-320","update-policy":"https:\/\/doi.org\/10.1144\/crossmark-policy","source":"Crossref","is-referenced-by-count":18,"title":["Formation of magnesium silicate hydrate cement in nature"],"prefix":"10.1144","volume":"175","author":[{"ORCID":"https:\/\/orcid.org\/0000-0002-3275-3870","authenticated-orcid":false,"given":"Lisa","family":"de Ruiter","sequence":"first","affiliation":[]},{"given":"H\u00e5kon","family":"Austrheim","sequence":"additional","affiliation":[]}],"member":"1881","published-online":{"date-parts":[[2017,11]]},"reference":[{"key":"e_1_3_3_2_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0012-8252(02)00106-X"},{"key":"e_1_3_3_3_1","doi-asserted-by":"publisher","DOI":"10.1144\/0016-76492012-011"},{"key":"e_1_3_3_4_1","doi-asserted-by":"publisher","DOI":"10.1029\/2006GL025681"},{"key":"e_1_3_3_5_1","doi-asserted-by":"publisher","DOI":"10.1016\/0016-7037(85)90228-5"},{"key":"e_1_3_3_6_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.geomorph.2006.06.016"},{"key":"e_1_3_3_7_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.chemgeo.2012.09.015"},{"key":"e_1_3_3_8_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.gca.2010.07.027"},{"key":"e_1_3_3_9_1","doi-asserted-by":"publisher","DOI":"10.1111\/j.1365-3121.2012.01083.x"},{"key":"e_1_3_3_10_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.gca.2008.07.002"},{"key":"e_1_3_3_11_1","doi-asserted-by":"publisher","DOI":"10.1016\/0009-2541(90)90084-K"},{"key":"e_1_3_3_12_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.palaeo.2004.10.017"},{"key":"e_1_3_3_13_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.cemconres.2004.06.022"},{"key":"e_1_3_3_14_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.apgeochem.2003.10.007"},{"key":"e_1_3_3_15_1","doi-asserted-by":"publisher","DOI":"10.1016\/0009-2541(87)90074-X"},{"key":"e_1_3_3_16_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.chemgeo.2013.05.020"},{"key":"e_1_3_3_17_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.eist.2015.10.001"},{"key":"e_1_3_3_18_1","doi-asserted-by":"publisher","DOI":"10.1016\/S0016-7037(97)00217-2"},{"key":"e_1_3_3_19_1","doi-asserted-by":"publisher","DOI":"10.1016\/S1474-8177(07)05011-5"},{"key":"e_1_3_3_20_1","doi-asserted-by":"publisher","DOI":"10.1093\/petrology\/egm021"},{"key":"e_1_3_3_21_1","doi-asserted-by":"publisher","DOI":"10.1346\/CCMN.2008.0560511"},{"key":"e_1_3_3_22_1","doi-asserted-by":"publisher","DOI":"10.1016\/0009-2541(77)90016-X"},{"key":"e_1_3_3_23_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.jhydrol.2017.04.059"},{"key":"e_1_3_3_24_1","doi-asserted-by":"publisher","DOI":"10.1086\/624619"},{"key":"e_1_3_3_25_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.ces.2007.09.052"},{"key":"e_1_3_3_26_1","doi-asserted-by":"publisher","DOI":"10.2113\/gscanmin.43.1.225"},{"key":"e_1_3_3_27_1","doi-asserted-by":"publisher","DOI":"10.1039\/FT9928800233"},{"key":"e_1_3_3_28_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.gca.2011.08.032"},{"key":"e_1_3_3_29_1","doi-asserted-by":"publisher","DOI":"10.1021\/es300403n"},{"key":"e_1_3_3_30_1","doi-asserted-by":"publisher","DOI":"10.1016\/j.ijsbe.2013.05.001"},{"key":"e_1_3_3_31_1","volume-title":"IPCC Special Report on Carbon Dioxide Capture and Storage","author":"IPCC.","year":"2005","unstructured":"IPCC. 2005. 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