作者: Takesi Nagata
DOI: 10.1007/BF00874778
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摘要: Characteristics of remanent magnetization an igneous rock under a uniaxial compression are divided into those the soft component and hard component. The irreversibly decreases with increase (σ) regardless whether axis σ is parallel or parpendicular to direction magnetization. changes reversibly σ: magnetic intensity increases when perpendicular magnetization, whereas it