Incompletely transformed serpentine-type phyllosilicates in the matrix of Antarctic CM chondrites

Author:

Akai Junji

Publisher

Elsevier BV

Subject

Geochemistry and Petrology

Reference29 articles.

1. Tubular form of interstratified mineral consisting of a serpentine-like layer plus two brucite-like sheets newly found in the Murchison (C2) meteorite;Akai;Mem. Natl. Inst. Polar Res., Spec. Issue,1980

2. High resolution electron microscopic characterization of phyllosilicates and finding of a new type with 11 Å structure in Yamato-74662;Akai;Mem. Natl. Inst. Polar Res., Spec. Issue,1982

3. Mineralogical study of matrix- and groundmass-phyllosilicates, and isolated olivines in Yamato- 791198 and Yamato-793321 —with special references to new finding of 14 Å chlorite in groundmass;Akai;Mem. Natl. Inst. Polar Res., Spec. Issue,1986

4. The dehydration of chrysotile in air and under hydrothermal conditions;Ball;Mineral. Mag.,1963

5. Matrix phyllosilicates and associated minerals in C2M carbonaceous chondrites;Barber;Geochim. Cosmochim. Acta,1981

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