Green’s Functions Outline

Attenuation Eikonal Eqn FD Solution to Eikonal Eqn Ray Tracing from Txz Traveltime Integral Ray Tracing from ODE All these records differ from those associated with terrestrial earthquakes in lacking S secondary or shear waves They also last for much longer than earthquakes up to an hour as though the Moon were ringing like a bell The bulk of the moonquakes originate from depths of 600 km or more attributed to the seismic signals bouncing back and forth in the low velocity surface layers

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