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Автор Vasconcelos, P. M.
Дата выпуска 1999
dc.description ▪ Abstract  Recent developments in the application of K-Ar and <sup>40</sup>Ar/<sup>39</sup>Ar dating of continental weathering process demonstrate the method's suitability for dating minerals present in weathering profiles. Alunite-group sulfates and hollandite-group manganese oxides, which often precipitate through weathering reactions, were first analyzed by the K-Ar method 30 years ago. Recently these minerals were shown to be suitable to <sup>40</sup>Ar/<sup>39</sup>Ar geochronology, despite their fine-grained habits. The bulk nature of the K-Ar technique and the complex mineral assemblages in weathering profiles restrict K-Ar dating of weathering processes. The single-crystal approach possible with the <sup>40</sup>Ar/<sup>39</sup>Ar method allows the study of weathering profiles where alunite- and hollandite-group minerals occur as minor phases. Step-heating analysis possible with the <sup>40</sup>Ar/<sup>39</sup>Ar method provides information about the Ar and K retention histories, the presence of hypogene contaminants, and possible <sup>39</sup>Ar recoil during sample irradiation. Fully automated, modern <sup>40</sup>Ar/<sup>39</sup>Ar systems enable analysis of several samples, providing a comprehensive weathering database. These results are useful in the study of continental paleoclimates and the geochemical, geomorphological, and tectonic histories of an area.
Формат application.pdf
Издатель Annual Reviews
Копирайт Annual Reviews
Название K-Ar AND <sup>40</sup>Ar/<sup>39</sup>Ar GEOCHRONOLOGY OF WEATHERING PROCESSES
DOI 10.1146/annurev.earth.27.1.183
Print ISSN 0084-6597
Журнал Annual Review of Earth and Planetary Sciences
Том 27
Первая страница 183
Последняя страница 229
Аффилиация Vasconcelos, P. M.; Department of Earth Sciences, University of Queensland, Brisbane, Queensland 4072, Australia; e-mail: paulo@sol.earthsciences.uq.edu.au

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