火成岩
地质学
纵波
变质岩
情态动词
矿物学
机械
地球物理学
波传播
光学
材料科学
物理
岩石学
复合材料
地球化学
标识
DOI:10.1029/jz065i004p01083
摘要
The velocity of compressional waves has been determined by measurement of travel time of pulses in specimens of rock at pressures to 10 kilobars and room temperature. Most of the samples, mainly igneous and metamorphic rocks, furnished three specimens oriented at right angles to one another. The present paper gives experimental details, modal analyses, and numerical tables of velocity as function of direction of propagation, initial density, and pressure. Discussion of various aspects of the measurements is reserved for part 2.
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