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A fireball flight with fragmentation witnessed from south-east to being many pieces at twilight sky.
It impacted at Kokubunji city, Kagawa prefecture, so it was called Kokubunji meteorite.
Maximum fragment recovered at Sakaide city when it named after.
Fresh broken inside is few blueish gray as general ordinary chondrite.
This color like with fresh concrete.
Most fragments keep fresh condition however photographed after years from fell.
Generally, brown rust appear on ordinary chondrite surface by inside ferrite.
Fusion crust is remnant of melted material interacted with atmosphere at high altitude.
A lot of ruggedness of the surface suggest fragmentation occured at low altitude.
This feature is not same as regmagripts.
|Kokubu No.1_A||Kokubu No.1_B||Kokubu No.1_C||Kokubu No.1_D||Nii No.5_A|
|Nii No.2_A||Nii No.1_J||Nii No.1_K||Nii No.4_A||Nii No.4_B||Nii No.5_B|
|Fuke No.1_A||Fuke No.1_B||Fuke No.1_C||Fuke No.1_C||Fuke No.1_G||Fuke No.1_F|
|Fuke No.1_E||Fuke No.2_A||Shinmyo No.3_A||Shinmyo No.3_B||Shinmyo No.4_A|
|Shinmyo No.1_A||Shinmyo No.1_B||Shinmyo No.1_C||Shinmyo No.1_D||Shinmyo No.1_E||Shinmyo No.2_A|
Kokubunji Junior high school : (in Japanese)