Moho depth determinations based on spectral-ratio analysis of NORSAR long-period P waves

Details Moho depth determinations based on spectral-ratio analysis of NORSAR long-period P waves Moho depth determinations based on spectral-ratio analysis of NORSAR long-period P waves

Sep 1977

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1977pepi...15...13b&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 15, Issue 1, p. 13-27.

Physics

19

Scientific paper

A model for a one-layered crust under the Norwegian Seismic Array in southeastern Norway has been determined by the application of the spectral-ratio method to long-period P waves recorded at the array's individual 22 long-period instrument sets. The model includes an average crustal velocity of 6.6 km/s and a depth to Moho which is 32-34 km in the eastern and southeastern part of the array and increases westward to about 38 km. Based on data simulations and observational material, it is concluded that the spectral-ratio method cannot be utilized to delineate the more detailed structure of the crust and upper mantle.

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