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- W2036691929 endingPage "1196" @default.
- W2036691929 startingPage "1177" @default.
- W2036691929 abstract "The past four years have witnessed the introduction of a variety of new instruments and methods for the study of the seismic structure of the oceanic crust and lithosphere. The application of these and existing tools has led to the discovery of a number of new phenomena and to a fuller understanding of the genesis and evolution of the oceanic ithosphere. Borehole seismic instrumentation has become more widely employed; ocean bottom seismographs, while generally decreasing in number, have become significantly more reliable and useful; and multichannel seismic systems have been employed in innovative experiments ranging from studies of fracture zones to the regular detection of magma chambers beneath rise axes. The techniques available for the analysis of seismic data have become more sophisticated. Waveforms collected in seismic experiments can now be used directly in constructing and evaluating seismic velocity models, and travel time data are regularly inverted directly for structure. Trial and error modeling has become increasingly unimportant. Marine seismologists are becoming increasingly involved in understanding the coupling between the ocean and the underlying oceanic lithosphere. This has led to a more complete understanding of seafloor noise processes and the partitioning of energy between acoustic and elastic waves." @default.
- W2036691929 created "2016-06-24" @default.
- W2036691929 creator A5077021409 @default.
- W2036691929 date "1987-07-01" @default.
- W2036691929 modified "2023-10-14" @default.
- W2036691929 title "Structure of the Earth: Oceanic crust and uppermost mantle" @default.
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