Illite-Age-Analysis (IAA) for the Dating of Shallow Faults: Prerequisites and Procedures for Improvement

Fault age determination using the illite-age-analysis (IAA) method for fault gouges has played a key role in providing absolute age information in tectonic evolution studies for the last 20 years. The accuracy and precision of the IAA method depend on (1) how to reasonably quantify the relative cont...

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Autores principales: Yungoo Song, Ho Sim
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Publicado: MDPI AG 2021
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spelling oai:doaj.org-article:62311452ac0349faa66de9d862486b8b2021-11-25T18:25:54ZIllite-Age-Analysis (IAA) for the Dating of Shallow Faults: Prerequisites and Procedures for Improvement10.3390/min111111622075-163Xhttps://doaj.org/article/62311452ac0349faa66de9d862486b8b2021-10-01T00:00:00Zhttps://www.mdpi.com/2075-163X/11/11/1162https://doaj.org/toc/2075-163XFault age determination using the illite-age-analysis (IAA) method for fault gouges has played a key role in providing absolute age information in tectonic evolution studies for the last 20 years. The accuracy and precision of the IAA method depend on (1) how to reasonably quantify the relative content of 1M/1M<sub>d</sub> illite generated from fault activity compared to detrital 2M<sub>1</sub> illite in the size fractions of the fault gouge, and (2) how to minimize the error factors in K-Ar or Ar-Ar dating analysis. XRD-based quantitative analysis of illite polytype has made great progress in accuracy by generating a simulated XRD pattern of 1M/1M<sub>d</sub> polytype using WILDFIRE© and full-pattern-fitting it with the XRD pattern measured from size fractions of the fault gauge. Nevertheless, the results of quantitative analysis of illite polytypes may vary depending on the sample state of the size fractions for XRD analysis, especially the preferred orientation due to the layered crystal structure of illite. In addition, the radiometric dating results may be distorted depending on the error factor of the dating method itself and on the mineral composition of the size fractions, that is, the presence of K-containing minerals such as biotite and K-feldspar other than illite. In this study, we reviewed previous studies that determined fault activity ages by applying IAA to fault gouges. From this, the prerequisites and recommendations for each of the five steps (particle size separation process, XRD analysis process, polytype quantification, radiometric dating, IAA plot) for improving the IAA method are summarized and presented. The continuous application of the improved IAA is expected to greatly contribute to the study of tectonic evolution through geological time.Yungoo SongHo SimMDPI AGarticleillite-age-analysis (IAA)fault datingpolytype quantificationWILDFIREmulti-focused XRDMineralogyQE351-399.2ENMinerals, Vol 11, Iss 1162, p 1162 (2021)
institution DOAJ
collection DOAJ
language EN
topic illite-age-analysis (IAA)
fault dating
polytype quantification
WILDFIRE
multi-focused XRD
Mineralogy
QE351-399.2
spellingShingle illite-age-analysis (IAA)
fault dating
polytype quantification
WILDFIRE
multi-focused XRD
Mineralogy
QE351-399.2
Yungoo Song
Ho Sim
Illite-Age-Analysis (IAA) for the Dating of Shallow Faults: Prerequisites and Procedures for Improvement
description Fault age determination using the illite-age-analysis (IAA) method for fault gouges has played a key role in providing absolute age information in tectonic evolution studies for the last 20 years. The accuracy and precision of the IAA method depend on (1) how to reasonably quantify the relative content of 1M/1M<sub>d</sub> illite generated from fault activity compared to detrital 2M<sub>1</sub> illite in the size fractions of the fault gouge, and (2) how to minimize the error factors in K-Ar or Ar-Ar dating analysis. XRD-based quantitative analysis of illite polytype has made great progress in accuracy by generating a simulated XRD pattern of 1M/1M<sub>d</sub> polytype using WILDFIRE© and full-pattern-fitting it with the XRD pattern measured from size fractions of the fault gauge. Nevertheless, the results of quantitative analysis of illite polytypes may vary depending on the sample state of the size fractions for XRD analysis, especially the preferred orientation due to the layered crystal structure of illite. In addition, the radiometric dating results may be distorted depending on the error factor of the dating method itself and on the mineral composition of the size fractions, that is, the presence of K-containing minerals such as biotite and K-feldspar other than illite. In this study, we reviewed previous studies that determined fault activity ages by applying IAA to fault gouges. From this, the prerequisites and recommendations for each of the five steps (particle size separation process, XRD analysis process, polytype quantification, radiometric dating, IAA plot) for improving the IAA method are summarized and presented. The continuous application of the improved IAA is expected to greatly contribute to the study of tectonic evolution through geological time.
format article
author Yungoo Song
Ho Sim
author_facet Yungoo Song
Ho Sim
author_sort Yungoo Song
title Illite-Age-Analysis (IAA) for the Dating of Shallow Faults: Prerequisites and Procedures for Improvement
title_short Illite-Age-Analysis (IAA) for the Dating of Shallow Faults: Prerequisites and Procedures for Improvement
title_full Illite-Age-Analysis (IAA) for the Dating of Shallow Faults: Prerequisites and Procedures for Improvement
title_fullStr Illite-Age-Analysis (IAA) for the Dating of Shallow Faults: Prerequisites and Procedures for Improvement
title_full_unstemmed Illite-Age-Analysis (IAA) for the Dating of Shallow Faults: Prerequisites and Procedures for Improvement
title_sort illite-age-analysis (iaa) for the dating of shallow faults: prerequisites and procedures for improvement
publisher MDPI AG
publishDate 2021
url https://doaj.org/article/62311452ac0349faa66de9d862486b8b
work_keys_str_mv AT yungoosong illiteageanalysisiaaforthedatingofshallowfaultsprerequisitesandproceduresforimprovement
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