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Please use this identifier to cite or link to this item: http://scholars.ntou.edu.tw/handle/123456789/26575
DC FieldValueLanguage
dc.contributor.authorChen, Yen-Yuen_US
dc.contributor.authorKao, Shao-, Ien_US
dc.contributor.authorChang, Ying-Juen_US
dc.date.accessioned2026-08-10T03:11:15Z-
dc.date.available2026-08-10T03:11:15Z-
dc.date.issued2026/2/7-
dc.identifier.issn1017-0839-
dc.identifier.urihttp://scholars.ntou.edu.tw/handle/123456789/26575-
dc.description.abstractAccurate 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.en_US
dc.language.isoEnglishen_US
dc.publisherSPRINGERNATUREen_US
dc.relation.ispartofTERRESTRIAL ATMOSPHERIC AND OCEANIC SCIENCESen_US
dc.subjectMicro-FTIRen_US
dc.subjectGeothermometryen_US
dc.subjectThermal maturityen_US
dc.subjectCoalen_US
dc.subjectRaman spectroscopyen_US
dc.subjectThermal historyen_US
dc.titleDevelopment of a rapid and high-precision micro-FTIR geothermometer for thermal history reconstruction of coal and rocksen_US
dc.typejournal articleen_US
dc.identifier.doi10.1007/s44195-026-00125-0-
dc.identifier.isiWOS:001711108700001-
dc.relation.journalvolume37en_US
dc.relation.journalissue1en_US
dc.relation.pages16en_US
dc.identifier.eissn2311-7680-
item.languageiso639-1English-
item.grantfulltextnone-
item.openairetypejournal article-
item.fulltextno fulltext-
item.cerifentitytypePublications-
item.openairecristypehttp://purl.org/coar/resource_type/c_6501-
crisitem.author.deptCollege of Ocean Science and Resource-
crisitem.author.deptInstitute of Earth Sciences-
crisitem.author.deptNational Taiwan Ocean University,NTOU-
crisitem.author.parentorgNational Taiwan Ocean University,NTOU-
crisitem.author.parentorgCollege of Ocean Science and Resource-
Appears in Collections:地球科學研究所
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