カンラン石の転位移動律速型粒界すべり:上部マントルの流動を支配する変形メカニズム Dislocation-accommodated grain boundary sliding: the major deformation mechanism of olivine in the Earth's upper mantle

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  • Annual Meeting of the Geological Society of Japan

    Annual Meeting of the Geological Society of Japan 2015(0), 213, 2015

    The Geological Society of Japan

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