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February 9, 2026Terrestrial Atmospheric and Oceanic Sciences0 citationsOpen Access

Development of a rapid and high-precision micro-FTIR geothermometer for thermal history reconstruction of coal and rocks

YCYen-Yu ChenNational Taiwan UniversitySKShao-I KaoKing's College LondonYCYing-Ju ChangNational Taiwan Ocean University

Key Points

  • The aim is to enhance the precision of thermal history reconstruction in geological materials using a micro-FTIR geothermometer.
  • Optimized an IR geothermometer protocol for analyzing thermal alteration in rocks and coal.
  • Conducted acid treatment to isolate organic components prior to analysis.
  • Utilized micro-Fourier Transform Infrared (Micro-FTIR) spectroscopy for sensitive temperature estimations.
  • Performed continuous heating experiments to assess thermal responses of samples.
  • Compared IR-derived temperatures with conventional methods like vitrinite reflectance and fission-track data.
  • Established a robust correlation between infrared thermal signatures and independent geothermometric controls.
  • Demonstrated the micro-FTIR technique's efficiency for reconstructing geological temperature histories.
  • Showed broader sample compatibility and improved precision for thermal event reconstructions.

Abstract

Abstract Accurate reconstruction of rock thermal history is prerequisite for understanding fundamental geological processes and assessing resource potential. Geothermometers provide critical constraints on the peak thermal exposure experienced by rocks or minerals during burial, diagenesis, or metamorphism. Conventional methods, such as vitrinite reflectance (VR) and fission-track (FT) thermochronology, yield valuable tem- perature data but are often constrained by time-intensive procedures, high resource consumption, and limitations in sample quantity or analytical spatial resolution. Micro-Fourier Transform Infrared (Micro-FTIR) Spectroscopy presents a viable alter- native for analyzing thermal alteration in geological media. This technique monitors infrared absorption changes in molecular bonds, revealing functional group transfor- mations that are acutely sensitive to thermal maturation and are effective proxies for reconstructing thermal history. This research optimizes an IR Geothermometer proto- col to address the intrinsic limitations of established techniques, thereby enhancing the precision of thermal event reconstruction. The methodology encompasses acid treatment for the isolation of organic components, Micro-FTIR analysis, and continuous heating experiments, resulting in broader sample compatibility and refined tempera- ture constraints. Methodological validation was performed by comparing IR-derived temperature estimates against VR data from coal samples and FT data from sedi- mentary and metamorphic rocks in Taiwan.The findings establish a robust empirical correlation between the observed IR thermal signatures and independent geothermo- metric controls, thereby confirming the technique’s efficacy for geological temperature history reconstruction. Utilizing the rapid spectral acquisition, high spatial resolu- tion, and capacity to register multiple thermal events inherent to IR spectroscopy, this technique offers an efficient, high-resolution methodology for thermal assessment in geological samples, with broad utility across resource exploration and petroleum geology.

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Cite This Study

Chen et al. (2026) studied this question.

synapsesocial.com/papers/69897a86f0ec2af6756e8babhttps://doi.org/10.1007/s44195-026-00125-0
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