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Enstatite from selected localities.

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    • Queen Maud Land
      • Queen Fabiola Mts
Ikeda Yukio (1988): Petrochemical study of the Yamato-691 enstatite chondrite (EH3) II: Descriptions and mineral compositions of unusual silicate-inclusions. Proceedings of the NIPR Symposium on Antarctic Meteorites 1, 14-37. [http://ci.nii.ac.jp/naid/110000029852/en/]; Nakamura-Messenger et al., (2011) The Formation of Wassonite: A New Titanium Monosulfide Mineral in the Yamato 691 Enstatite Chondrite: Workshop on Formation of the First Solids in the Solar System: LPI Contribution No. 1639, p. 9091. (Nov 2011)
Kato, Y., Sekine, T., Kayama, M., Miyahara, M., & Yamaguchi, A. (2017). High‐pressure polymorphs in Yamato‐790729 L6 chondrite and their significance for collisional conditions. Meteoritics & Planetary Science, 52(12), 2570-2585.
Itoh, S., Rubin, A. E., Kojima, H., Wasson, J. T. & Yurimoto, H. (2003) Amoeboid Olivine Aggregates and AOA-bearing Chondrule from Y-81020 CO3.0 Chondrite: Distribution of Oxygen and Magnesium Isotopes (abstract): Lunar and Planetary Science Conference XXXIII, abstract #1490. (Mar 2003).
Lin, Y. & Kimura, M. (1998) Petrographic and mineralogical study of new EH melt rocks and a new enstatite chondrite grouplet: Meteoritics & Planetary Science 33(3): 501-511. (May 1998)
Ohgo, S., Mishima, M., Endo, M., Ninagawa, K., & Nishido, H. (2017). Cathodoluminescence color zonation in the Antarctic meteorite (enstatite chondrite) of Yamato 86004. Geochronometria, 44(1), 136-141.
 
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