イカ石
(イカアイト から転送)
出典: フリー百科事典『ウィキペディア(Wikipedia)』 (2024/06/04 08:12 UTC 版)
イカ石(イカせき[3]、ikaite)、もしくはイカアイトは、鉱物(炭酸塩鉱物)の一種。化学組成は CaCO3·6H2O(炭酸カルシウム6水和物)、結晶系は単斜晶系。
- ^ Ikaite (英語), MinDat.org, 2012年3月20日閲覧。 (英語)
- ^ Ikaite (英語), WebMineral.com, 2012年3月20日閲覧。 (英語)
- ^ 松原聰、宮脇律郎『日本産鉱物型録』東海大学出版会〈国立科学博物館叢書〉、2006年、57頁。ISBN 978-4-486-03157-4。
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- ^ Bethelsen, A. (1962). “On the geology of the country around Ivigtut, SW Greenland”. Geologische Rundschau 52: 260–280.
- ^ Emeleus, C. H. (1964). “The Grønnedal-Ikka Alkaline Complex, South Greenland: The structure and geological history of the complex.”. Grønlands Geologiske Undersøgelse.
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- ^ Buchardt, B., Israelson, C., Seaman, P., and Stockmann, G. (2001). “The Ikaite tufa towers in Ikka Fjord, SW Greenland: Formation by mixing of seawater and alkaline spring water”. Journal of Sedimentary Research 71: 176–189. doi:10.1306/042800710176.
- ^ Suess, E., Balzer, W., Hesse, K.-F., Muller, P.J., Ungerer, C.A., and Wefer, G. (1982). “Calcium carbonate hexahydrate from organic rich sediments of the Antarctic shelf: precursors of glendonites”. Science 216 (4550): 1128–1131. doi:10.1126/science.216.4550.1128. PMID 17808501.
- ^ Greinert, J.; Derkachev, A. (2004). “Glendonites and methane-derived Mg-calcites in the Sea of Okhotsk, Eastern Siberia: implications of a venting-related ikaite/glendonite formation”. Marine Geology 204: 129–144. doi:10.1016/S0025-3227(03)00354-2.
- ^ a b c 伊藤俊彦「北海道,シオワッカ冷泉産のikaite」『岩鉱』第91巻第6号、日本岩石鉱物鉱床学会、1996年、209-219頁、doi:10.2465/ganko.91.209、ISSN 0914-9783、NAID 10002087929。
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- ^ Bischoff, J. L., Stine, S., Rosenbauer, R. J., Fitzpatrick, J. A., Stafford Jr, T. W., (1993). “Ikaite precipitation by mixing of shoreline springs and lake water, Mono Lake, California, USA”. Geochimica et Cosmochimica Acta 57 (16): 3855–3856. doi:10.1016/0016-7037(93)90339-X.
- ^ a b Dickens, B.; Brown, W.E. (1970). “The crystal structure of calcium carbonate hexahydrate at ~120°C”. Inorganic Chemistry 9 (3): 480–486. doi:10.1021/ic50085a010.
- ^ a b Swainson, I.P.; Hammond, R.P. (2003). “Hydrogen bonding in ikaite, CaCO3.6H2O”. Mineralogical Magazine (The Mineralogical Society) 67 (3): 555–562. doi:10.1180/0026461036730117. ISSN 0026-461X.
- ^ Hesse, K. -F., Kuppers, H., Suess, E., (1983). “Refinement of the structure of Ikaite, CaCO3.6H2O”. Zeitschrift fur Kristallographie 163 (3–4): 227–231. doi:10.1524/zkri.1983.163.3-4.227.
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- ^ Bischoff; J.L, Fitzpatrick, J.A.; Rosenbauer, R.J. (1992). “The solubility and stabilization of ikaite (CaCO3.6H2O) from 0° to 25°C”. Journal of Geology 101: 21–33.
- ^ Marland, G. (1975). “The stability of CaCO3.6H2O (ikaite)”. Geochimica et Cosmochimica Acta 39: 83–91. doi:10.1016/0016-7037(75)90186-6.
- ^ a b E.S. Dana (1884). “A crystallographic study of the thinolite of Lake Lahontan”. U.S. Geological Survey Bulletin (Washington, D.C.: U.S. Government Printing Office) (12): 429–450.
- ^ Kaplan, M.E. (1979). “Calcite pseudomorphs (pseudogaylusite, jarrowite, thinolite, glendonite, gennoishi) in sedimentary rocks. The origin of pseudomorphs (in Russian)”. Lithology and Mineral Resources 5: 125–141.
- ^ Council, T. C.; Bennett, P. C. (1993). “Geochemistry of ikaite formation at Mono Lake, California: Implications for the origin of tufa mounds”. Geology 21 (11): 971–974. doi:10.1130/0091-7613(1993)021<0971:GOIFAM>2.3.CO;2.
- ^ Browell, E. J. J. (1860). “Description and analysis of an undescribed mineral from Jarrow Slake”. Tyneside Naturalists Field Club V: 103–104.
- ^ Shearman, D.J.; Smith, A.J. (1985). “Ikaite, the parent mineral of jarrowite-type pseudomorphs”. Proceedings of the Geological Association, London 96 (4): 305–314. doi:10.1016/S0016-7878(85)80019-5.
- ^ Stein, C.L.; Smith, A.J. (1985). “Authigenic carbonate nodules in the Nankai Trough, Site 583”. Initial reports of the DSDP 87: 659–668.
- ^ Kennedy,G.L.; Hopkins, D.M.; Pickthorn, W.J. (1987年), Ikaite, the glendonite precursor, in estuarine sediments at Barrow, Arctic Alaska, Annual Meeting Abstract Program, vol. 9, Geological Society of America, p. 725
- ^ Swainson, I.P.; Hammond, R.P. (2001). “Ikaite, CaCO3.6H2O: Cold comfort for glendonites as palaeothermometers”. American Mineralogist ([[:en:Mineralogical Society of America|]]) 86: 1530–1533. ISSN 0003-004X.
- ^ Shearman, D.J.; McGugan, A.;Stein, C.;Smith, A.J. (1989). “Ikaite, CaCO3.6H2O, precursor of the thinolites in the Quaternary tufas and tufa mounds of the Lahontan and Mono Lake Basins, western United States”. Geological Society of America Bulletin 101 (7): 913–917. doi:10.1130/0016-7606(1989)101<0913:ICOPOT>2.3.CO;2.
- ^ Whiticar, M.J.; Suess, E. (1998). “The cold carbonate connection between Mono Lake, California and the Bransfield Strait, Antarctica”. Aquatic Geochemistry 4 (3/4): 429–454. doi:10.1023/A:1009696617671.
- ^ Schubert, C.J.; Nunberg, D.; Scheele, N.; Pauer, F.; Kriews, M. (1997). “13C isotope depletion in ikaite crystal: evidence for methane release from the Siberian shelves?”. Geo-Marine Letters 17 (2): 169–174. doi:10.1007/s003670050023.
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