鉱物学雜誌
Online ISSN : 1883-7018
Print ISSN : 0454-1146
ISSN-L : 0454-1146
コンドライトの成因とレオロジー
北村 雅夫
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ジャーナル フリー

1990 年 19 巻 3 号 p. 177-179

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Chondrites were formed in small planets, where convection did not occur Therefore, rheological processes such as bracciation and shock deformation were essential in the formation of parent bodies of chondrites. Origin of chondrules were also reviewed with reference of shock melting.

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