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Some Seismic Profiles near the Western End of the Puerto Rico Trench

机译:波多黎各海沟西端附近的一些地震剖面

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摘要

A cooperative program of seismic refraction profiling was completed in the vicinity of the Puerto Rico Trench by Hudson Laboratories, Woods Hole, Lamont, and Texas A. & M. Profiles completed near the western end of the Trench were analyzed at Hudson Laboratories. Five seismic layers are indicated below the water layer. The thickness/velocity relationships are as follows: 5.1 km of 1.5 km/sec. (water); 1 km of 1.7 km/sec. (sediment); 1.5 km of 3 km/sec. (metamorphics?); 2 km of 5.5 km/sec. (basement); and 2 km of 7.1 km/sec. (high speed basement). Below these, typical Moho velocities of 8.1 km/sec. were measured. Total depth to Moho ranges from 9 to 12 km below sea level, the greatest variation occurring in the basement layers. The least depth was measured 65 miles north of the Puerto Rico Trench.
机译:Hudson Laboratories,Woods Hole,Lamont和Texas A.&M在波多黎各海沟附近完成了一项地震折射剖面合作计划。在Hudson Laboratories分析了海沟西端附近完成的剖面。在水层下方指示了五个地震层。厚度/速度关系如下:1.5 km / sec的5.1 km。 (水); 1公里为1.7公里/秒。 (沉淀); 1.5 km of 3 km / sec。 (变质?); 2公里(5.5公里/秒)。 (地下室);和2公里(7.1公里/秒)。 (高速地下室)。在这些之下,典型的Moho速度为8.1 km / sec。被测量。到莫霍面的总深度在海平面以下9至12公里,最大的变化发生在地下层。在波多黎各海沟以北65英里处测得的最小深度。

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