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Cross joint - Oudansetsuri (English spelling) cross joint
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A joint that is perpendicular or nearly perpendicular to the flow line caused by the intrusion of a rock mass and perpendicular to the ground surface. It is considered to be a typical example of a tension joint that is perpendicular to the primary flow plane and perpendicular to tensile stress. Source: Asakura Publishing Dictionary of Petrology Information |
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岩体の貫入による流線に直角かそれに近く，かつ地表に垂直な節理．一次的な流理面に垂直で，引張り応力に垂直にできる張力節理（tension joint）の代表的なものと考えられている． 出典 朝倉書店岩石学辞典について 情報 |
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