Olivine annealed up to 1500 C: changes traced by polarised IR reflectance and magnetization

Fuente: arXiv
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Main Authors: Smith, Daniel, Narbutis, Donatas, Huang, Hsin-Hui, Zanon, Philipp, Boschen, Michael, Vongsvivut, Jitraporn, Appadoo, Dominique, Ng, Soon Hock, Mu, Haoran, Katkus, Tomas, Le, Nguyen Hoai An, Kapsaskis, Dan, Herries, Andy I. R., Anand, Vijayakumar, Ryu, Meguya, Morikawa, Junko, Juodkazis, Saulius
Format: Preprint
Published: 2026
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_version_ 1866918435539124224
author Smith, Daniel
Narbutis, Donatas
Huang, Hsin-Hui
Zanon, Philipp
Boschen, Michael
Vongsvivut, Jitraporn
Appadoo, Dominique
Ng, Soon Hock
Mu, Haoran
Katkus, Tomas
Le, Nguyen Hoai An
Kapsaskis, Dan
Herries, Andy I. R.
Anand, Vijayakumar
Ryu, Meguya
Morikawa, Junko
Juodkazis, Saulius
author_facet Smith, Daniel
Narbutis, Donatas
Huang, Hsin-Hui
Zanon, Philipp
Boschen, Michael
Vongsvivut, Jitraporn
Appadoo, Dominique
Ng, Soon Hock
Mu, Haoran
Katkus, Tomas
Le, Nguyen Hoai An
Kapsaskis, Dan
Herries, Andy I. R.
Anand, Vijayakumar
Ryu, Meguya
Morikawa, Junko
Juodkazis, Saulius
contents Spectral analysis at the infrared (IR) spectral range is introduced with assignment of synthetic red-green-blue (RGB) colours defined by adjustable wavelength and bandwidth. The RGB bands were selected at the phase-specific absorbance A or reflectance R bands of olivine and related materials, which can be formed via high temperature annealing (HTA) of natural minerals up to 1500 C. Natural olivines were collected from quarry at volcanic site in Mortlake, Victoria, Australia and spectrally characterised during IR-THz spectroscopy beamtime experiments at Australian Synchrotron. Phase changes in HTA natural olivines were traced by correlation of optical IR 4-polarisation spectroscopy, X-ray energy dispersive spectroscopy and magnetisation. After HTA, olivine samples were magnetized via precipitation of Fe-rich oxides.
format Preprint
id arxiv_https___arxiv_org_abs_2604_07356
institution arXiv
publishDate 2026
record_format arxiv
spellingShingle Olivine annealed up to 1500 C: changes traced by polarised IR reflectance and magnetization
Smith, Daniel
Narbutis, Donatas
Huang, Hsin-Hui
Zanon, Philipp
Boschen, Michael
Vongsvivut, Jitraporn
Appadoo, Dominique
Ng, Soon Hock
Mu, Haoran
Katkus, Tomas
Le, Nguyen Hoai An
Kapsaskis, Dan
Herries, Andy I. R.
Anand, Vijayakumar
Ryu, Meguya
Morikawa, Junko
Juodkazis, Saulius
Geophysics
Materials Science
Spectral analysis at the infrared (IR) spectral range is introduced with assignment of synthetic red-green-blue (RGB) colours defined by adjustable wavelength and bandwidth. The RGB bands were selected at the phase-specific absorbance A or reflectance R bands of olivine and related materials, which can be formed via high temperature annealing (HTA) of natural minerals up to 1500 C. Natural olivines were collected from quarry at volcanic site in Mortlake, Victoria, Australia and spectrally characterised during IR-THz spectroscopy beamtime experiments at Australian Synchrotron. Phase changes in HTA natural olivines were traced by correlation of optical IR 4-polarisation spectroscopy, X-ray energy dispersive spectroscopy and magnetisation. After HTA, olivine samples were magnetized via precipitation of Fe-rich oxides.
title Olivine annealed up to 1500 C: changes traced by polarised IR reflectance and magnetization
topic Geophysics
Materials Science
url https://arxiv.org/abs/2604.07356