Chang'E-5 regolith (Lunar: basalt)
Pang R., Yang J., Du W., Zhang A., Liu S., and Li R. 2022. New Occurrence of Seifertite and Stishovite in Chang’E‐5 Regolith. Geophysical Research Letters, e2022GL098722.
Fritz J, Greshake A., Klementova M., Wirth R., Palatinus L., Trønnes R. G., Fernandes V. A., Böttger U. , and Ferrière, L. 2020. Donwilhelmsite, [CaAl4Si2O11], a new lunar high-pressure Ca-Al-silicate with relevance for subducted terrestrial sediments. American Mineralogist, 105, 1704–1711.
NWA 2995 (Lunar: feldspathic breccia)
Zhang A. C., Jiang Q. T., Tomioka N., Guo Y. J., Chen J. N., Li Y., Sakamoto N., and Yurimoto H. Widespread tissintite in strongly shock‐lithified lunar regolith breccias. Geophysical Research Letters 48:e2020GL091554.
Zhang A. C., Jiang Q. T., Tomioka N., Guo Y. J., Chen J. N., Li Y., Sakamoto N., and Yurimoto H. 2021. Widespread tissintite in strongly shock‐lithified lunar regolith breccias. Geophysical Research Letters 48:e2020GL091554.
NWA 8182 (Lunar: feldspathic breccia)
Zhang A. C., Jiang Q. T., Tomioka N., Guo Y. J., Chen J. N., Li Y., Sakamoto N., and Yurimoto H. 2021. Widespread tissintite in strongly shock‐lithified lunar regolith breccias. Geophysical Research Letters 48:e2020GL091554.
Zhang A. C., Jiang Q. T., Tomioka N., Guo Y. J., Chen J. N., Li Y., Sakamoto N., and Yurimoto H. 2021. Widespread tissintite in strongly shock‐lithified lunar regolith breccias. Geophysical Research Letters 48:e2020GL091554.
Zhang A. C., Jiang Q. T., Tomioka N., Guo Y. J., Chen J. N., Li Y., Sakamoto N., and Yurimoto H. Widespread tissintite in strongly shock‐lithified lunar regolith breccias. Geophysical Research Letters 48:e2020GL091554.
NWA 10253: feldspathic breccia)
Zhang A. C., Jiang Q. T., Tomioka N., Guo Y. J., Chen J. N., Li Y., Sakamoto N., and Yurimoto H. Widespread tissintite in strongly shock‐lithified lunar regolith breccias. Geophysical Research Letters 48:e2020GL091554.
NWA 10272 (Lunar: feldspathic breccia)
Zhang A. C., Jiang Q. T., Tomioka N., Guo Y. J., Chen J. N., Li Y., Sakamoto N., and Yurimoto H. 2021. Widespread tissintite in strongly shock‐lithified lunar regolith breccias. Geophysical Research Letters 48:e2020GL091554.
Zhang A. C., Jiang Q. T., Tomioka N., Guo Y. J., Chen J. N., Li Y., Sakamoto N., and Yurimoto H. 2021. Widespread tissintite in strongly shock‐lithified lunar regolith breccias. Geophysical Research Letters 48:e2020GL091554.
NWA 11273 (Lunar: feldspathic breccia)
Zhang A. C., Jiang Q. T., Tomioka N., Guo Y. J., Chen J. N., Li Y., Sakamoto N., and Yurimoto H. 2021. Widespread tissintite in strongly shock‐lithified lunar regolith breccias. Geophysical Research Letters 48:e2020GL091554.
NWA 13967 (Lunar: feldspathic breccia)
Wittmann A., Kroemer C. R., Wadhwa M., Sharp T. G., Van Soest M., Martin T., and Goepfert, T. 2025. Tissintite‐II in Lunar Meteorite Northwest Africa 13967: Implications for the High Pressure/Temperature Mineralogy of the Lunar Regolith. Meteoritics & Planetary Science.
Barrat J. A., Chaussidon M., Bohn M., Gillet Ph., Göpel C., and Lesourd M. 2005. Lithium behavior during cooling of a dry basalt: An ion-microprobe study of the lunar meteorite Northwest Africa 479 (NWA 479). Geochimica et Cosmochimica Acta 69: 5597–5609.
Miyahara M., Kaneko S., Ohtani E., Sakai T., Nagase T., Kayama M., Nishido H., and Hirao N. 2013. Discovery of seifertite in a shocked lunar meteorite. Nature Communications 4:1737.
Ohtani E., Ozawa S., Miyahara M., Ito Y., Mikouchi T., Kimura M., Arai T., Sato K., and Hiraga K. 2011. Coesite and stishovite in a shocked lunar meteorite, Asuka-881757, and impact events in lunar surface. Proceedings of the National Academy of Sciences of the USA 108:463–466.
Zhang A. C., Hsu W.-B., Floss C., Li X.-H., Li Q.-L., Liu Y., and Taylor L. A. 2010. Petrogenesis of lunar meteorite Northwest Africa 2977: Constrains from in situ microprobe results. Meteoritics & Planetary Science 45:1929–1947.
NWA 2727 (Lunar: basalt/gabbro breccia)
Kayama M., Tomioka N., Ohtani E., Seto Y., Nagaoka H., Götze, J., Miyake, A., Ozawa S., Sekine T., Miyahara M., Tomeoka K., Matsumoto M., Shoda N., Hirao N., and Kobayashi T. 2018. Discovery of moganite in a lunar meteorite as a trace of H2O ice in the Moon’s regolith. Science advances, 4:eaar4378.
SaU 169 (Lunar: rigolith breccia)
Xing W., Lin Y., Zhang C., Zhang M., Hu S., Hofmann, B. A., Sekine T., Xiao L., and Gu L. 2020. Discovery of Reidite in the Lunar Meteorite Sayh al Uhaymir 169. Geophysical Research Letters, e2020GL089583.
Apollo 15299 (Lunar: regolith breccia)
Kaneko S., Miyahara M., Ohtani E., Arai T., Hirao N., and Sato K. 2015. Discovery of stishovite in Apollo 15299 sample. American Mineralogist 100:1308–1311.
DaG 735 (Maritian: shergottite)
Miyahara M., Ohtani E., Ozawa S., Kimura M., El Goresy A., Sakai T., Nagase T., Hiraga K., Hirao N., and Ohishi Y. 2011. Natural dissociation of olivine to (Mg,Fe)SiO3 perovskite and magnesiowüstite in a shocked Martian meteorite. Proceedings of the National Academy of Sciences of the U.S.A.108:5999–6003.
DaG 670 (Maritian: shergottite)
Greshake A., Fritz J., Böttger U., and Goran D. 2013. Shear-induced ringwoodite formation in the Martian shergottite Dar al Gani 670. Earth and Planetary Science Letters 375:383–394.
EETA 79001 (Maritian: shergottite)
Walton-Hauck E. L. 2012. The occurrence of ringwoodite in shock veins of the Elephant Moraine A79001 shergottite. 43rd Lunar and Planetary Science Conference:1697.pdf.
GRV 020090 (Maritian: shergottite)
Lin Y., Feng L., and Hu S. 2011. High pressure mineral assemblages in the lherzolitic Shergottite Grove Mountains (GRV) 020090. Japan Geoscience Union meeting 2011, PPS003–11.
Lin Y., Feng L., Hu S., Zhang J., and Hao J. 2012. NanoSIMS study of shock-induced melt veins in the enriched lherzolitic Shergottite Grove Mountains (GRV) 020090. Japan Geoscience Union Meeting 2012. PPS05–03.
NWA 480 (Maritian: shergottite)
El Goresy A., Gillet Ph., Miyahara M., Ohtani E., Ozawa S., Beck P., and Montagnac G. 2013. Shock-induced deformation of Shergottites: Shock–pressures and perturbations of magmatic ages on Mars. Geochimica et Cosmochimica Acta 101:233–262.
NWA 856 (Maritian: shergottite)
Beck P., Gillet Ph., Gautron L., Daniel I., and El Goresy A. 2004. A new natural high-pressure (Na,Ca)-hexaluminosilicate [(CaxNa1-x)Al3+xSi3-xO11] in shocked Martian meteorites. Earth and Planetary Science Letters 219:1–12.
El Goresy A., Gillet Ph., Miyahara M., Ohtani E., Ozawa S., Beck P., and Montagnac G. 2013. Shock-induced deformation of Shergottites: Shock–pressures and perturbations of magmatic ages on Mars. Geochimica et Cosmochimica Acta 101:233–262.
Tschauner O., Ma C., Spray J. G., Greenberg E., and Prakapenka V. B. 2021: Stöfflerite, (Ca,Na)(Si,Al)4O8 in the hollandite structure: A new high-pressure polymorph of anorthite from martian meteorite NWA 856. American Mineralogist 106: 650–655.
NWA 1068 (Maritian: shergottite)
Beck P., Gillet Ph., Gautron L., Daniel I., and El Goresy A. 2004. A new natural high-pressure (Na,Ca)-hexaluminosilicate [(CaxNa1-x)Al3+xSi3-xO11] in shocked Martian meteorites. Earth and Planetary Science Letters 219:1–12.
NWA 2975 (Maritian: shergottite)
He Q., Xiao L., Balta J. B., Baziotis I. P., Hsu W., and Guan Y. 2015. Petrography and geochemistry of the enriched basaltic shergottite Northwest Africa 2975. Meteoritics & Planetary Science 50:2024–2044.
NWA 4468 (Maritian: shergottite)
Boonsue S. and Spray J. 2012. Shock-induced phase transformations in melt pockets within Martian meteorite NWA 4468. Spectroscopy Letters 45:127–134.
NWA 7755 (Maritian: shergottite)
Wang S. Z., Zhang A. C., Pang R. L., Chen J. N., Gu L. X., and Wang R. C. 2017. Petrogenesis and shock metamorphism of the enriched lherzolitic shergottite Northwest Africa 7755. Meteoritics & Planetary Science 52:2437–2457.
NWA 7397 (Maritian: shergottite)
Yoshida M., Miyahara M., Suga H., Yamaguchi Al., Tomioka N., Sakai T., Ohfuji H., Maeda F., Ohhira I., Ohtani E., Kamada S., Ohhigashi T., Inagaki Y., Kodama Y., and Hirao N. 2021. Elucidation of impact event recorded in the lherzolitic shergottite NWA 7397. Meteoritics & Planetary Science (in press)
NWA 8657 (Maritian: shergottite)
Hu S., Li Y., Gu L., Tang X., Zhang T., Yamaguchi A. Lin Y., and Changela, H. 2020. Discovery of coesite from the martian shergottite Northwest Africa 8657. Geochimica et Cosmochimica Acta, 286: 404–417.
NWA 8705 (Maritian: shergottite)
Zhang T., Hu S., Wang N., Lin Y., Gu L., Tang X., Zou X., and Zhang M. 2021. Formation mechanisms of ringwoodite and wadsleyite; clues from the Martian meteorite Northwest Africa 8705, 73, 165.
Los Angeles (Maritian: shergottite)
Beck P., Gillet Ph., Gautron L., Daniel I., and El Goresy A. 2004. A new natural high-pressure (Na,Ca)-hexaluminosilicate [(CaxNa1-x)Al3+xSi3-xO11] in shocked Martian meteorites. Earth and Planetary Science Letters 219:1–12.
SaU 005 (Maritian: shergottite)
Beck P., Gillet Ph., Gautron L., Daniel I., and El Goresy A. 2004. A new natural high-pressure (Na,Ca)-hexaluminosilicate [(CaxNa1-x)Al3+xSi3-xO11] in shocked Martian meteorites. Earth and Planetary Science Letters 219:1–12.
Chassigny (Martian: chassignite)
Malavergne V., Guyot F., Benzerara K., and Martinez I. 2001. Description of new shock-induced phases in the Shergotty, Zagami, Nakhla and Chassigny meteorites. Meteoritics & Planetary Sciences 36:1297–1305.
El Goresy A., Dera P., Sharp T. G., Prewitt C. T., Chen M., Dubrovinsky L., Wopenka B., Boctor N. Z., and Hemley R. J. 2008. Seifertite, a dense orthorhombic polymorph of silica from the Martian meteorites Shergotty and Zagami. European Journal of Mineralogy 20:523–528.
Fritz J. and Greshake A. 2009. High-pressure phases in an ultramafic rock from Mars. Earth and Planetary Science Letters 288:619–623.
NWA 2737 (Maritian: chassignite)
Van de Moortèle B., Reynard B., McMillan P. F., Wilson M., Beck P., Gillet P., and Jahn S. 2007. Shock-induced transformation of olivine to a new metastable (Mg,Fe)2SiO4 polymorph in Martian meteorites. Earth and Planetary Science Letters 261:469–475.
Shergotty (Maritian: shergottite)
Sharp T. G., El Goresy A., Wopenka B., and Chen M. 1999. A post-stishovite SiO2 polymorph in the meteorite Shergotty: Implications for impact events. Science 284:1511–1513.
El Goresy A., Dubrovinsky L., Sharp T. G., Saxena S. K., and Chen M. 2000. A monoclinic post-stishovite polymorph of silica in the Shergotty meteorite. Science 288:1632–1634.
Malavergne V., Guyot F., Benzerara K., and Martinez I. 2001. Description of new shock-induced phases in the Shergotty, Zagami, Nakhla and Chassigny meteorites. Meteoritics & Planetary Science 36:1297–1305.
El Goresy A., Dera P., Sharp T. G., Prewitt C. T., Chen M., Dubrovinsky L., Wopenka B., Boctor N. Z., and Hemley R. J. 2008. Seifertite, a dense orthorhombic polymorph of silica from the Martian meteorites Shergotty and Zagami. European Journal of Mineralogy 20:523–528.
Bläß U. W. 2013. Shock-induced formation mechanism of seifertite in shergottites. Physics and Chemistry of Minerals 40:425–437.
Ma C., Tschauner O., Beckett J. R., and Prakapenka, V. B. 2025. New high‐pressure Fe‐Ti oxide minerals in the Shergotty Martian meteorite: Feiite, Fe22+(Fe2+ Ti4+) O5, liuite, FeTiO3, and tschaunerite,(Fe2+)(Fe2+ Ti4+) O4. Meteoritics & Planetary Science, 60:375–379.
Tissint (Maritian: shergottite)
Walton E. L., Sharp T. G., Hu J., and Filiberto J. 2014. Heterogeneous mineral assemblages in martian meteorite Tissint as a result of a recent small impact event on Mars. Geochimica et Cosmochimica Acta 140:334–348.
Baziotis I. P., Yang L., Paul S., De Carli H., Melosh J., McSween H. Y., Bodnar R. J., and Taylor L. A. 2013. The Tissint Martian meteorite as evidence for the largest impact excavation. Nature Communications doi: 10.1038/ncomms2414.
Ma C., Tschauner O., Beckett J. R., Liu Y., Rossman G. R., Zhuravlev K, Prakapenka V., Dera P., and Taylor L. A. 2015. Tissintite, (Ca,Na,□)AlSi2O6, a highly-defective, shock-induced, high-pressure clinopyroxene in the Tissint martian meteorite. Earth and Planetary Science Letters 422:194–205.
Miyahara M., Ohtani E., El Goresy A., Ozawa S., and Gillet Ph. 2016. Phase transition processes of olivine in the shocked Martian meteorite Tissint: Clues to origin of ringwoodite-, bridgmanite- and magnesiowüstite-bearing assemblages. Physics of the Earth and Planetary Interiors 259:18–28.
Ma C., Tschauner O., Beckett J. R., Liu Y., Greenberg E., and Prakapenka V. B. 2019. Chenmingite, FeCr2O4 in the CaFe2O4-type structure, a shock-induced, high-pressure mineral in the Tissint martian meteorite. American Mineralogist 104:1521–1525.
Yamato 000047 (Maritian: shergottite)
Imae N. and Ikeda Y. 2010. High-pressure polymorphs of magnesian orthopyroxene from a shock vein in the Yamato-000047 lherzolitic shergottite. Meteoritics & Planetary Sciences 45:43–54.
Zagami (Maritian: shergottite)
Langenhorst F. and Poirier J. P. 2000. `Eclogitic' minerals in a shocked basaltic meteorite. Earth and Planetary Science Letters 176:259–265.
Langenhorst F. and Poirier J. P. 2000. Anatomy of black veins in Zagami: clues to the formation of high-pressure phases. Earth and Planetary Science Letters 184:37–55.
Beck P., Gillet Ph., Gautron L., Daniel I., and El Goresy A. 2004. A new natural high-pressure (Na,Ca)-hexaluminosilicate [(CaxNa1-x)Al3+xSi3-xO11] in shocked Martian meteorites. Earth and Planetary Science Letters 219:1–12.
Beck P., Gillet P., El Goresy A., and Mostefaoui S. 2005. Timescales of shock processes in chondritic and martian meteorites. Nature 435:1071–1074.
Bläß U. W. 2013. Shock-induced formation mechanism of seifertite in shergottites. Physics and Chemistry of Minerals 40:425–437.
Ma, C., Tschauner, O., Beckett, J. R., Rossman, G. R., Prescher, C., Prakapenka, V. B., Bachtel, H. A., and MacDowell, A. 2018. Liebermannite, KAlSi3O8, a new shock‐metamorphic, high‐pressure mineral from the Zagami Martian meteorite. Meteoritics & Planetary Science 53:50–61.
Gu L., Hu S., Anand M., Tang X., Ji J., and Zhang B. 2021. Occurrence of tuite and ahrensite in Zagami and their significance for shock-histories recorded in martian meteorites. American Mineralogist (in press).
NWA 8159 (Maritian: augite basalt)
Sharp T. G., Walton E. L., Hu J., and Agee C. 2019. Shock conditions recorded in NWA 8159 martian augite basalt with implications for the impact cratering history on Mars. Geochimica et Cosmochimica Acta 246:197–212.
Béréba (Eucrite: monomict breccia)
Miyahara M., Ohtani E., Yamaguchi A., Ozawa S., Sakai T., and Hirao N. 2014. Discovery of coesite and stishovite in eucrite. Proceedings of the National Academy of Sciences of the U.S.A. 111:10939–10942.
Padvarninkai (Eucrite: monomict breccia)
Miyahara M., Yamaguchi A., Ohtani E., Tomioka N., and Kodama Y. 2021. Complicated pressure–temperature path recorded in the eucrite Padvarninkai. Meteoritics & Planetary Science doi.org/10.1111/maps.13724.
NWA 2650 (Eucrite: monomict breccia)
Chen D. L., Zhang A. C., Pang R. L., Chen J. N., and Li Y. 2019. Shock‐induced phase transformation of anorthitic plagioclase in the eucrite meteorite Northwest Africa 2650. Meteoritics & Planetary Science 54:1548–1562.
Pang R.-L., Zhang A.-C., Wang S.-Z., Wang R.-C., and Yurimoto H. 2016. High-pressure minerals in eucrite suggest a small source crater on Vesta. Scientific Reports 6: 26063, doi:10.1038/srep26063.
Pang R. L., Harries D., Pollok K., Zhang A. C., and Langenhorst F. 2018. Vestaite, (Ti4+Fe2+) Ti4+3O9, a new mineral in the shocked eucrite Northwest Africa 8003. American Mineralogist, 103:1502–1511.
Pang R. L., Harries D., Pollok K., Zhang A. C., and Langenhorst, F. 2019. Unique mineral assemblages of shock-induced titanium-rich melt pockets in eucrite Northwest Africa 8003. Geochemistry, 79:125541.
NWA 10658 (Eucrite: polymict breccia)
Fudge C., Sharp T. G., Hu J., Ma C., Tschauner O., and Wittmann A. 2018. Characterization of a new high-pressure assemblage after anorthitic plagioclase in polymict eucrite Northwest Africa 10658. 49th LPSC XXXXVIII, 2417.pdf.
Miyamoto M., Matsuda J. I., and Ito K. 1988. Raman spectroscopy of diamond in ureilite and implication for the origin of diamond. Geophysical Research Letters 15:1445–1448.
Nakamuta Y, and Aoki Y. 2000. Mineralogical evidence for the origin of diamond in ureilites. Meteoritics & Planetary Science 35:487–493.
Nakamuta Y. and Aoki Y. 2000. Mineralogical evidence for the origin of diamond in ureilites. Meteoritics & Planetary Science, 35:487–493.
Miyahara M., Ohtani E., El Goresy A., Lin Y., Feng L., Zhang J. C., Gillet P., Nagase T., Muto J., and Nishijima M. 2015. Unique large diamonds in a ureilite from Almahata Sitta 2008 TC3 asteroid. Geochimica et Cosmochimica Acta 163:14–26.
Nabiei F., Badro J., Dennenwaldt T., Oveisi E., Cantoni M., Hébert C., El Goresy A., Barrat, J., and Gillet P. 2018. A large planetary body inferred from diamond inclusions in a ureilite meteorite. Nature Communications 9:1327.
Lipschutz M. E. 1964. Origin of diamonds in the ureilites. Science 143:1431–1434.
Frontier Mountain 01012 (Ureilite)
Barbaro A., Domeneghetti M. C., Fioretti A. M., Alvaro M., and Nestola F. 2023. Carbon polymorphs in Frontier Mountain ureilitic meteorites: A correlation with increasing the degree of shock?. Earth and Planetary Science Letters, 614:118201.
Frontier Mountain 01088 (Ureilite)
Barbaro A., Domeneghetti M. C., Fioretti A. M., Alvaro M., and Nestola F. 2023. Carbon polymorphs in Frontier Mountain ureilitic meteorites: A correlation with increasing the degree of shock?. Earth and Planetary Science Letters, 614:118201.
Frontier Mountain 01089 (Ureilite)
Barbaro A., Domeneghetti M. C., Fioretti A. M., Alvaro M., and Nestola F. 2023. Carbon polymorphs in Frontier Mountain ureilitic meteorites: A correlation with increasing the degree of shock?. Earth and Planetary Science Letters, 614:118201.
Frontier Mountain 97013 (Ureilite)
Barbaro A., Domeneghetti M. C., Fioretti A. M., Alvaro M., and Nestola F. 2023. Carbon polymorphs in Frontier Mountain ureilitic meteorites: A correlation with increasing the degree of shock?. Earth and Planetary Science Letters, 614:118201.
Lipschutz M. E. 1964. Origin of diamonds in the ureilites. Science 143:1431–1434.
Marvin U. B., and Wood J. A. 1972. The Haverö ureilite: petrographic notes. Meteoritics & Planetary Science 7:601–610.
Nestola, F.,Goodrich, C. A., Morana, M., Barbaro, A., Jakubek, R. S., Christ, O., Brenker, F. E., Domeneghetti, M. C., Dalconi, M. C., Alvaro, M., Fioretti, A. M., Litasov, K. D., Fries, M. D., Leoni, M., Casati, N. P. M., Jenniskens, P., and Shaddad, M. H. 2020. Impact shock origin of diamonds in ureilite meteorites. Proceedings of the National Academy of Sciences 117: 25310–25318.
Lipschutz M. E. 1964. Origin of diamonds in the ureilites. Science 143:1431–1434.
Gibson Jr E. K. 1976. Nature of the carbon and sulfur phases and inorganic gases in the Kenna ureilite. Geochimica et Cosmochimica Acta 40:1459–1464.
Nakamuta Y. and Aoki Y. 2000. Mineralogical evidence for the origin of diamond in ureilites. Meteoritics & Planetary Science, 35:487–493.
Barbaro A., Domeneghetti M. C., Litasov K. D., Ferrière L., Pittarello L., Christ O., Lorenzon S., Alvaro M, and Nestola F. 2021. Origin of micrometer-sized impact diamonds in ureilites by catalytic growth involving Fe-Ni-silicide: The example of Kenna meteorite. Geochimica et Cosmochimica Acta 309:286–298.
Marvin U. B., and Wood J. A. 1972. The Haverö ureilite: petrographic notes. Meteoritics & Planetary Science 7:601–610.
Ferroir T., Dubrovinsky L., El Goresy A., Simionovici A., Nakamura T., and Gillet P. 2010. Carbon polymorphism in shocked meteorites: Evidence for new natural ultrahard phases. Earth and Planetary Science Letters 290:150–154.
Barbaro, A., Nestola, F., Pittarello, L., Ferrière, L., Murri, M., Litasov, K. D., Christ, O., Alvaro, M., and Domeneghetti, M. C. 2022. Characterization of carbon phases in Yamato 74123 ureilite to constrain the meteorite shock history. American Mineralogist, 107:377–384.
Nakamuta Y. and Aoki Y. 2000. Mineralogical evidence for the origin of diamond in ureilites. Meteoritics & Planetary Science, 35:487–493.
Nakamuta Y. and Aoki Y. 2000. Mineralogical evidence for the origin of diamond in ureilites. Meteoritics & Planetary Science, 35:487–493.
Britvin S. N., Shilovskikh V. V., Pagano R., Vlasenko N. S., Zaitsev A. N., Krzhizhanovskaya M. G., Lozhkin M. S, Zolotarev A. A., and Gurzhiy V. V., 2019. Allabogdanite, the high-pressure polymorph of (Fe,Ni)2P, a stishovite-grade indicator of impact processes in the Fe–Ni–P system. Scientific Reports 9:1047.
Litasov K. D. and Podgornykh N. M. 2017. Raman spectroscopy of various phosphate minerals and occurrence of tuite in the Elga IIE iron meteorite. Journal of Raman Spectroscopy 48:DOI:10.1002/jrs.5119
Holtstam D., Broman C., Söderhielm J., and Zetterqvist A. 2003. First discovery of stishovite in an iron meteorite. Meteoritics & Planetary Science 38:1579–1583.
Britvin S. N., Rudashevsky N. S., Krivovichev S. V., Burns P. C., and Polekhovsky Y. S. 2002. Allabogdanite, (Fe,Ni)2P, a new mineral from the Onello meteorite: The occurrence and crystal structure. American Mineralogist 87:1245–1249.
Britvin S. N., Shilovskikh V. V., Pagano R., Vlasenko N. S., Zaitsev A. N., Krzhizhanovskaya M. G., Lozhkin M. S, Zolotarev A. A., and Gurzhiy V. V. 2019. Allabogdanite, the high-pressure polymorph of (Fe,Ni)2P, a stishovite-grade indicator of impact processes in the Fe–Ni–P system. Scientific Reports 9:1047.
Santa Catharina (iron, IAB-ungrouped)
Britvin S. N., Shilovskikh V. V., Pagano R., Vlasenko N. S., Zaitsev A. N., Krzhizhanovskaya M. G., Lozhkin M. S, Zolotarev A. A., and Gurzhiy V. V. 2019. Allabogdanite, the high-pressure polymorph of (Fe,Ni)2P, a stishovite-grade indicator of impact processes in the Fe–Ni–P system. Scientific Reports 9:1047.