Figure 1.
ORN and observed seismicity over a 2-month period. The events have been located using the HYP code and a preliminary velocity model (see Table S1 in supporting information). Red dots denote events that have been used for the calculation of the P-wave minimum 1-D model, meanwhile events presented by a black dot were excluded from the calculation for quality reasons. The depth always denotes depth beneath seafloor. All stations have been set to a depth of 0 km, to keep the calculation simple. The histogram in the lower-right corner gives a count of earthquakes per 1 km-interval. The total number of events for the depth interval 0–1 km is 56. Multibeam bathymetry from Ranero et al. (2003).

ORN and observed seismicity over a 2-month period. The events have been located using the HYP code and a preliminary velocity model (see Table S1 in supporting information). Red dots denote events that have been used for the calculation of the P-wave minimum 1-D model, meanwhile events presented by a black dot were excluded from the calculation for quality reasons. The depth always denotes depth beneath seafloor. All stations have been set to a depth of 0 km, to keep the calculation simple. The histogram in the lower-right corner gives a count of earthquakes per 1 km-interval. The total number of events for the depth interval 0–1 km is 56. Multibeam bathymetry from Ranero et al. (2003).

Close
This Feature Is Available To Subscribers Only

Sign In or Create an Account

Close

This PDF is available to Subscribers Only

View Article Abstract & Purchase Options

For full access to this pdf, sign in to an existing account, or purchase an annual subscription.

Close