本文详细研究了台湾澎湖列岛上地幔幔源包体的变形结构、组构和橄榄石位错构造。
This paper deals with deformation textures, petrofabrics and dislocation microstructures of olivine from the mantle-derived xenoliths in the Penghu Islands, Taiwan.
本区上地幔变形事件和热结构特征表明，福建东部和台湾澎湖列岛一带具有十分相似的上地幔流变学特征。
Deformation events and thermal textures of the upper mantle in this region show that Fujian and the Penghu Islands are characterized by a similar rheological state of the upper mantle.
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