Shaking Layers are shaking intensity maps generated minutes after a NZ earthquake. These products are available for earthquake events of magnitude 4 or higher. Using the instrumental data from GeoNet’
The GFZ Potsdam started a log interpretation study in cooperation with the Technical University of Aachen. As a first result, the logged profile allows for a subdivision of the lithological profile in
Higher abundance of greigite during glacial intervals also coincides with small increases of the S content (Fig. 11B). Greigite levels in glacial sediments cannot be correlated between cores (Fig. 12)
