dì zhì xué jiā / tōng guò / fēn xī / piàn má yán / de / chéng fèn / lái / tuī cè / dì qiào / yùn dòng / de / lì shǐ地质学家通过分析片麻岩的成分来推测地壳运动的历史。Geologists analyze the composition of gneiss to infer the history of crustal movement.