An inclusion of ALH-77004: A possible surface regolith of L chondrite parent body

スポンサーリンク

概要

• 論文の詳細を見る

• An inclusion in ALH-77004 (H4 chondrite) consists of four different constituents with varying degree of recrystallization; (1) moderately to highly recrystallized lithic and chondrule fragments (fayalite-rich group), (2) unequilibrated chondrules (fayalite-poor group), (3) fine-grained dark clastic matrix, and (4) particles of Fe-Ni metal, troilite, and chromite. From petrological examinations of these constituents, it is suggested that the inclusion was a surface regolith of the L chondrite parent body formed by repetitive impact cratering processes extended to various depths of the body.

• 国立極地研究所の論文

著者

• Matsunami Satoshi

  Geological Institute Faculty Of Science University Of Tokyo

関連論文

• An inclusion of ALH-77004: A possible surface regolith of L chondrite parent body
• The chemical compositions and textures of matrices and chondrule rims of eight unequilibrated ordinary chondrites: A preliminary report

スポンサーリンク