Three-dimensional structure of the Earth from splitting in free-oscillation spectra

Observations of splitting in free oscillations spectra can be used to constrain the three-dimensional distribution of heterogeneity in the Earth. Modes sampling mainly the Earth's mantle are compatible with the distributions of mantle heterogeneity inferred from P-wave travel times. The anomalo...

תיאור מלא

מידע ביבליוגרפי
Main Authors: Giardini, D, Li, X, Woodhouse, J
פורמט: Journal article
שפה:English
יצא לאור: 1987