רינגוודיט
הערות שוליים

↑  מינרל נדיר שהתגלה לראשונה בכדור הארץ מצביע על אפשרות למאגר מים תת-קרקעי עצום, אוניברסיטת אלברטה, מרץ 2014 (באנגלית)
↑  Chen.
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↑  David L. Kohlstedt; Hans Keppler; David C. Rubie (1996). "Solubility of water in the alpha, beta, and gamma phases of (Mg,Fe)2SiO4". Contributions to Mineralogy and Petrology. 123 (4): 345–357. Bibcode:1996CoMP..123..345K. doi:10.1007/s004100050161.
↑  J. R. Smyth; C. M. Holl; D. J. Frost; S. D. Jacobsen; F. Langenhorst; C. A. McCammon (2003). "Structural systematics of hydrous ringwoodite and water in Earth's interior". American Mineralogist. 88 (10): 1402–1407. Bibcode:2003AmMin..88.1402S. doi:10.2138/am-2003-1001.
↑  A. Kavner (2003). "Elasticity and strength of hydrous ringwoodite at high pressure". Earth and Planetary Science Letters. 214 (3–4): 645–654. Bibcode:2003E&PSL.214..645K. doi:10.1016/s0012-821x(03)00402-3.
↑  Y. Xu; D.J. Weider; J.Chen; M.T. Vaughan; Y. Wang; T. Uchida (2003). "Flow-law for ringwoodite at subduction zone conditions". Physics of the Earth and Planetary Interiors. 136 (1–2): 3–9. Bibcode:2003PEPI..136....3X. doi:10.1016/s0031-9201(03)00026-8.
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↑  Richard A. Lovett (12 במרץ 2014). "Tiny diamond impurity reveals water riches of deep Earth". Nature. doi:10.1038/nature.2014.14862. ארכיון מ-11 במרץ 2021. נבדק ב-1 בספטמבר 2014. {{cite journal}}:  (עזרה)
↑  D. G. Pearson; F. E. Brenker; F. Nestola; J. McNeill; L. Nasdala; M. T. Hutchison; S. Matveev; K. Mather; G. Silversmit; S. Schmitz; B. Vekemans (13 במרץ 2014). "Hydrous mantle transition zone indicated by ringwoodite included within diamond" (PDF). Nature. 507 (7491): 221–224. Bibcode:2014Natur.507..221P. doi:10.1038/nature13080. PMID 24622201. ארכיון (PDF) מ-22 בספטמבר 2017. נבדק ב-4 בדצמבר 2019. {{cite journal}}:  (עזרה)
1 2 3  Sample, Ian (12 במרץ 2014). "Rough diamond hints at vast quantities of water inside Earth". The Guardian. ארכיון מ-20 במרץ 2014. נבדק ב-6 בדצמבר 2014. {{cite news}}:  (עזרה)
↑  "sample of the week: ringwoodite". super/collider. אורכב מ-המקור ב-28 בדצמבר 2014. נבדק ב-6 בדצמבר 2014. {{cite web}}:  (עזרה)
↑  Andy Coghlan (21 יוני 2014). "Massive 'ocean' discovered towards Earth's core". New Scientist. ארכיון מ-11 בדצמבר 2019. נבדק ב-2 בדצמבר 2019. {{cite journal}}:  (עזרה)
↑  Schmandt, Brandon; Jacobsen, Steven D.; Becker, Thorsten W.; Liu, Zhenxian; Dueker, Kenneth G. (13 ביוני 2014). "Dehydration melting at the top of the lower mantle". Science. 344 (6189): 1265–1268. Bibcode:2014Sci...344.1265S. doi:10.1126/science.1253358. PMID 24926016. {{cite journal}}:  (עזרה)
↑  The structure of spinel structure is more accurately described as F43m, according to N. W. Grimes;  et al. (8 אפר' 1983). "New Symmetry and Structure for Spinel". Proceedings of the Royal Society of London. Series A, Mathematical and Physical Sciences. 386 (1791): 333–345. Bibcode:1983RSPSA.386..333G. doi:10.1098/rspa.1983.0039. JSTOR 2397417. {{cite journal}}:  (עזרה)
↑  Price, Geoffrey D.; Parker, Stephen C. (באפריל 1984). "Computer simulations of the structural and physical properties of the olivine and spinel polymorphs of Mg2SiO4". Physics and Chemistry of Minerals. 10 (5): 209–216. Bibcode:1984PCM....10..209P. doi:10.1007/BF00309313. {{cite journal}}:  (עזרה)
↑  Smyth, J.R. and T.C. McCormick (1995).
↑  Ye, Y.; Brown, D.A.; Smyth, J. R.; Panero, W.R.; Jacobsen, S.D.; Chang, Y.-Y.; Townsend, J.P.; Thomas, S.M.; Hauri, E.; Dera, P.; Frost, D.J. (2012). "Compressibility and thermal expansion study of hydrous Fo100 ringwoodite with 2.5(3) wt% H2O" (PDF). American Mineralogist. 97: 573–582. doi:10.2138/am.2012.4010. אורכב מ-המקור (PDF) ב-2014-06-29.
↑  Ye, Y.; Brown, D.A.; Smyth, J. R.; Panero, W.R.; Jacobsen, S.D.; Chang, Y.-Y.; Townsend, J.P.; Thomas, S.M.; Hauri, E.; Dera, P.; Frost, D.J. (2012). "Compressibility and thermal expansion study of hydrous Fo100 ringwoodite with 2.5(3) wt% H2O" (PDF). American Mineralogist. 97: 573–582. doi:10.2138/am.2012.4010. אורכב מ-המקור (PDF) ב-2014-06-29.
↑  Katsura, T., Yokoshi, S., Song, M., Kawabe, K., Tsujimura, T., Kubo, A., Ito, E., Tange, Y., Tomioka, N., Saito, K. and Nozawa, A. (2004). "Thermal expansion of Mg2SiO4 ringwoodite at high pressures". Journal of Geophysical Research: Solid Earth. 109 (B12): B12. Bibcode:2004JGRB..10912209K. doi:10.1029/2004JB003094.{{cite journal}}:  תחזוקה - ציטוט: multiple names: authors list (link)
↑  Nishihara, Y., Takahashi, E., Matsukage, K. N., Iguchi, T., Nakayama, K., & Funakoshi, K. I. (2004). "Thermal equation of state of (Mg0.91,Fe0.09)2SiO4 ringwoodite". Physics of the Earth and Planetary Interiors. 143: 33–46. Bibcode:2004PEPI..143...33N. doi:10.1016/j.pepi.2003.02.001.{{cite journal}}:  תחזוקה - ציטוט: multiple names: authors list (link)
↑  Armentrout, M., & Kavner, A. (2011). "High pressure, high temperature equation of state for Fe2SiO4 ringwoodite and implications for the Earth's transition zone". Geophysical Research Letters. 38 (8): n/a. Bibcode:2011GeoRL..38.8309A. doi:10.1029/2011GL046949.{{cite journal}}:  תחזוקה - ציטוט: multiple names: authors list (link)
↑  Lingemann C. M. and D. Stöffler 1994.
↑  Keppler, H.; Smyth, J.R. (2005). "Optical and near infrared spectra of ringwoodite to 21.5 GPa". American Mineralogist. 90: 1209–1214. doi:10.2138/am.2005.1908.