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The document discusses a study on the elemental analysis of foraminifera from ocean sediment cores to understand past ocean temperatures and conditions. It details the cleaning and measurement processes for trace elements, as well as the significance of Mg/Ca ratios in paleotemperature estimation. Additionally, it presents findings from seismic reflection data in the northern Cascadia subduction zone, highlighting the characteristics of megathrust shear zones and their implications for earthquake activity.

Author

serpzen

Language

EN