Figure 17: Vertical component spectra for the three broadband seismometer configurations deployed on the OSNPE (seafloor, buried and borehole) and the Kipapa GSN station on Oahu are compared with high and low noise spectral models based on land observations. From 20mHz to 100mHz the borehole and buried sensors in the ocean are as quiet as any land sensor.
Retun to the 2003 Fall AGU Poster
THIRD PARTY BOREHOLE SEISMIC EXPERIMENTS DURING THE OCEAN DRILLING PROGRAM
Created on December 10, 2003 by Tom Bolmer