Description
Shore-based X-ray Fluorescence (XRF), IODP Expedition 395 Site U1602 X-ray fluorescence (XRF) is a rapid, non-destructive technique for determining qualitative and quantitative changes in chemical composition. In the shore-based laboratory at Scripps Institution of Oceanography, University of California, San Diego, an Avaatech XRF Core Scanner was used to measure a large number of spots along the length of a core. Spots are typically irradiated at multiple conditions to excite and measure a wide range of elements. The peak intensity changes (we do not provide concentrations) are then used to help recognize and define major chemo-stratigraphic units without the need for destructive sampling.
Date made available | Mar 21 2025 |
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Publisher | ZENODO |
Data Monitor Categories
- contourite drifts
- Northern Hemisphere glaciation
- Reykjanes Mantle and Climate
- mantle plume
- climate record
- IODP
- oceanic gateways
- Expedition 395
- JOIDES Resolution
- Earth in Motion
- Eirik Drift
- Earth Connections
- International Ocean Discovery Program
- Site U1602