Figure 9
From: New perspectives on Solid Earth Geology from Seismic Texture to Cooperative Inversion
Images showing wireline logs plotted76 over color coded seismic textural cluster distribution along the trace of the Kevitsa drillhole 2. The image includes plots of velocity, density, gamma and conductivity along with Ni percent. Point A marks the change from cluster I which has the second highest textural entropy centroid. Point A also coincides with a change from lower to higher velocity and density. The petrophysics in Kevitsa drillhole 2 is more complex than that for Kevitsa drillhole 1 where there is negligible mineralization (barren rock). That is, high Ni and high conductivity are not bound within one particular textural cluster.
