中文摘要:文章归纳了地壳上地幔各种岩石矿物的速度特征。长英质岩石的上地壳具有较低的 P波速度；各类花岗质岩石到云英闪长质片麻杂岩组成的中部地壳P波速度为 6.4～6.6 km/s；由石榴石、角闪石、辉石或橄榄石组成的下陆壳P波速度最大，达到了6.8～7.0 km/s，当 P波速度大于7.3 km/s时则应有相当高的榴辉岩和超镁铁岩的高速组分。在地壳下面的岩石圈地幔主要由橄榄岩质岩石（超镁铁岩）组成，地震波纵波速度达到8.0 km/s以上。
Abstract:The authors sum up the P-wave velocities of rock-forming minerals in the crust and the upper mantle. The felsic rocks that compose the upper crust have lower P-wave velocity, the P-wave velocity of the granitic and greisen-dioritic gneiss complexes that compose the middle crust is 6.4~6.6 km/s, and the lower crust rocks composed of garnet, amphibole, pyroxene and olivine have the highest P-wave velocity: 6.8~7.0 km/s. When P-wave velocity is higher than 7.3 km/s, there must exist high velocity components like eclogites and ultramafic rocks. The velocity of peridotite that makes up lithosphere mantle (ultramafic rocks) is higher than 8.0 km/s.
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基金项目:地质大调查综合研究项目“中国成矿体系与成矿评价”（K1.4）
引用文本：
彭聪，邓晋福，邱瑞照.2004.地壳上地幔地震波速度结构和岩石学解释综述[J].矿床地质,23(Z):13~18.2004.Seismic Wave Velocity Structure of Crust and Upper Mantle and Petrological Interpretation[J].Mineral Deposits23(Z):13~18
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