全部 标题 作者
关键词 摘要

OALib Journal期刊
ISSN: 2333-9721
费用:99美元

查看量下载量

相关文章

更多...

The Anecdote of Liuite
—In View of the Progress of Modern Technology, There Might Be No More New Minerals to Be Found on the Earth after another Half a Century

DOI: 10.4236/aa.2023.133016, PP. 245-252

Keywords: Liuite, Lingunite, Earth Mantle, Most Abundant Mineral

Full-Text   Cite this paper   Add to My Lib

Abstract:

Liuite (FeTiO3 with an orthorhombic perovskite structure) is a new mineral approved by the Commission on New Minerals, Nomenclature and Classification (CNMNC) of the International Mineralogical Association (IMA) in November 2018. It was named after my family name, Liu, because I am the first person who synthesized/identified this new material in my laboratory in 1975 at the Research School of Earth Sciences, Australian National University. Since 1991, however, liuite has been proposed or suggested to name for other minerals by various Earth scientists from various countries. The scenario of the intriguing story is presented here.

References

[1]  Birch, F. (1952). Elasticity and Constitution of the Earth’s Interior. Journal of Geophysical Research, 57, 227-286.
https://doi.org/10.1029/JZ057i002p00227
[2]  Birch, F., & LeComte, P. (1960). Temperature-Pressure Plane for Albite Composition. American Journal of Science, 258, 209-217.
https://doi.org/10.2475/ajs.258.3.209
[3]  Chao, E. C. T., Fahey, J. J., & Littler, J. (1962). Stishovite, SiO2, a Very High Pressure New Mineral from Meteor Crater, Arizona. Journal of Geophysical Research, 67, 419-421.
https://doi.org/10.1029/JZ067i001p00419
[4]  Chao, E. C. T., Shoemaker, E. M., & Madsen, B. M. (1960). First Natural Occurrence of Coesite. Science, 132, 220-222.
https://doi.org/10.1126/science.132.3421.220
[5]  Coes Jr., L. (1953). A New Dense Crystalline Silica. Science, 118, 131-132.
https://doi.org/10.1126/science.118.3057.131
[6]  Gillet, P., Chen, M., Dubrovinsky, L. S., & El Goresy, A. (2000). Natural NaAlSi3O8-Hol-landite in the Shocked Sixiangkou Meteorite. Science, 287, 1633-1636.
https://doi.org/10.1126/science.287.5458.1633
[7]  Huang, E. (1991). The Most Abundant Mineral in Earth—Liusite. Science Monthly, 22, 143. (In Chinese)
[8]  Kawai, N., Tachimori, M., & Ito, E. (1974). A High Pressure Hexagonal form of MgSiO3. Proceedings of the Japan Academy, 50, 378-380.
https://doi.org/10.2183/pjab1945.50.378
[9]  Liu, L.-G. (1974). Silicate Perovskite from Phase Transformations of Pyrope-Garnet at High Pressure and Temperature. Geophysical Research Letters, 1, 277-280.
https://doi.org/10.1029/GL001i006p00277
[10]  Liu, L.-G. (1975a). Post-Oxide Phases of Olivine and Pyroxene and Mineralogy of the Mantle. Nature, 258, 510-512.
https://doi.org/10.1038/258510a0
[11]  Liu, L.-G. (1975b). High Pressure Phase Transformations and Compressions of Ilmenite and Rutile, I. Experimental Results. Physics of the Earth and Planetary Interiors, 10, 167-176.
https://doi.org/10.1016/0031-9201(75)90035-7
[12]  Liu, L.-G. (1976). The High Pressure Phases of MgSiO3. Earth and Planetary Science Letters, 31, 200-208.
https://doi.org/10.1016/0012-821X(76)90212-0
[13]  Liu, L.-G. (1977). Ilmenite-Type Solid Solutions between MgSiO3 and Al2O3 and Some Structural Systematics among Ilmenite Compounds. Geochimica et Cosmochimica Acta, 41, 1355-1361.
https://doi.org/10.1016/0016-7037(77)90078-3
[14]  Liu, L.-G. (1978). High Pressure Phase Transformations of Albite, Jadeite and Nepheline. Earth and Planetary Science Letters, 37, 438-444.
https://doi.org/10.1016/0012-821X(78)90059-6
[15]  Liu, L.-G. (1982). Chemical Inhomogeneity of the Mantle: Geochemical Considerations. Geophysical Research Letters, 9, 124-126.
https://doi.org/10.1029/GL009i002p00124
[16]  Ma, C., Tschauner, O., Beckett, J. R., & Prakapenka, V. (2021). Discovery of Feiite (Fe2+2(Fe2+Ti4+)O5) and Liuite (GdFeO3-Type FeTiO3), Two New Shock Induced, High-Pressure Minerals in the Martian Meteorite Shergotty. In 52nd Lunar and Planetary Science Conference (LPI Contribution No. 2548).
[17]  Ramsdell, L. S. (1955). The Crystallography of ‘Coesite’. American Mineralogist, 40, 975-982.
[18]  Sharp, T. G., Lingemann, C. M., Dupas, C., & Stoffler, D. (1997). Natural Occurrence of MgSiO3-Ilmenite and Amorphized MgSiO3-Perovskite in a Shocked L Chondrite. Science, 277, 352-355.
https://doi.org/10.1126/science.277.5324.352
[19]  Sosman, R. B. (1954). New High-Pressure Phases of Silica. Science, 119, 738-739.
https://doi.org/10.1126/science.119.3099.738
[20]  Stishov, S. M., & Popova, S. V. (1961). A New Dense Modification of Silica. Geokhimoya, 10, 837-839.
[21]  Tomioka, N., & Fujino, K. (1997). Natural (Mg,Fe)SiO3-Ilmenite and-Perovskite in the Tenham Meteorite. Science, 277, 1084-1086.
https://doi.org/10.1126/science.277.5329.1084
[22]  Tschauner, O., Ma, C., Beckett, J. R., Prescher, C., & Prakapenka, V. B. (2014). Discovery of Bridgmanite, the Most Abundant Mineral in Earth, in a Shocked Meteorite. Science, 346, 1100-1102.
https://doi.org/10.1126/science.1259369
[23]  Zoltai, T., & Buerger, M. J. (1959). The Crystal Structure of Coesite, the Dense, High-Pressure Form of Silica. Zeitschrift für Kristallographie, 111, 129-141.
https://doi.org/10.1524/zkri.1959.111.1-6.129

Full-Text

comments powered by Disqus

Contact Us

service@oalib.com

QQ:3279437679

WhatsApp +8615387084133

WeChat 1538708413