Japan Geoscience Union Meeting 2014

Presentation information

Poster

Symbol P (Space and Planetary Sciences) » P-PS Planetary Sciences

[P-PS22_1PO1] Planetary processes from meteorites and experimental works

Thu. May 1, 2014 6:15 PM - 7:30 PM Poster (3F)

Convener:*Kimura Makoto(Faculty of Science, Ibaraki University), Eiji Ohtani(Department of Earth and Planetary Materials Science, Graduate School of Science, Tohoku University), Masaaki Miyahara Masaaki(Department of Earth and Planetary Systems Science, Graduate School of Science, Hiroshima University)

6:15 PM - 7:30 PM

[PPS22-P04] Petrologic type from plagioclase size distribution

Takehiro KAWASAKI1, *Makoto KIMURA1, Takaaki NOGUCHI1 (1.Faculty of Science, Ibaraki University)

Keywords:ordinary chondrite, petrologic type, plagioclase, thermal metamorphism

Ordinary chondrites are classified into petrologic types 3-6, reflecting thermal metamorphism. One of the criteria to classify types 5 and 6 is the size distribution of plagioclase. The size, 50 microns, has been commonly used to classify types 5 and 6. However, no any statistic study for plagioclase size has been conducted. Here we measured the size distribution, and discuss the classification of types 5 and 6. We studied 26 thin sections of types 5 and 6 from the H, L, and LL chondrite groups. Our study indicates that plagioclase of 50 microns are commonly encountered both in types 5 and 6. However, plagioclase of 80-100 microns is more abundant in type 6 than type 5. We also noticed that the size distribution of plagioclase in H6 is similar to that in type H5. The different criteria to classify H from L and LL are necessary.