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Application of Raman Imaging in UHPM Research

  • Andrey V. KorsakovEmail author
Chapter
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Part of the Springer Series in Surface Sciences book series (SSSUR, volume 66)

Abstract

Crustal-derived rocks can be subducted to mantle depth and metamorphosed at ultra-high pressure conditions (>2.6 GPa and 600 \(^{\circ }\)C), which are defined by the presence of coesite . Findings of diamond in metamorphic rocks further extended the upper pressure limit for crustal rocks (>4.0 GPa and 900–1000 \(^{\circ }\)C). Almost all ultra-high pressure mineral-indicators occur as small relics and Raman spectroscopy is a very powerful tool for the identification of these relics. Despite the significant progress in Raman imaging, this technique remains underestimated in ultra-high pressure research. In this chapter several examples of Raman imaging applied in ultra-high pressure petrology are summarised and discussed.

Notes

Acknowledgements

This study was supported by a grant from the Russian Science Foundation (RSF 15-17-30012).

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© Springer International Publishing AG 2018

Authors and Affiliations

  1. 1.Sobolev Institute of Geology and MineralogySiberian Branch, Russian Academy of SciencesNovosibirskRussian Federation

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