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EGU2018-16538.pdf

EGU2018-16538.pdf
Preview of EGU2018-16538
🔗 Source: meetingorganizer.copernicus.org
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Summary

OH-defects in quartz can serve as an archive for its host rock's formation, and detrital quartz from different sources can show distinctive distributions of OH defect contents, quantifiable using IR-spectroscopy. Application of this technique to river sands from southwestern Japan separates them into two provenances based on OH-defect content: OH-defect poor quartz in central Honshu and a wider range of OH-defect contents in Shikoku. The lower OH-defect contents in central Honshu are hypothesized to result from erosion of rock from lower crustal levels following the collision of the Izu- and Honshu arcs, and the OH-defect signal is traceable throughout the sediment record, making it a legitimate tool for provenance analysis.

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Description

OH-defects in quartz can serve as an archive for its host rock's formation, and detrital quartz from different sources can show distinctive distributions of OH...

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  • File Format: PDF
  • File Size: 32 KB
  • Pages: 1
  • Language: EN
  • Total Downloads: 206
  • Last Updated: 1 week ago

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