Rates of Weathering Layer Development: A Review of Studies on Weathering Rind, Weathering Crust, and Rock Varnish
Author:
Affiliation:
1. Department of Science and Engineering, Saitama University
Publisher
Tokyo Geographical Society
Subject
Materials Chemistry
Link
https://www.jstage.jst.go.jp/article/jgeography/126/4/126_126.473/_pdf
Reference82 articles.
1. Anderson, L.W. and Anderson, D.S. (1981): Weathering rinds on quartzarenite clasts as a relative-age indicator and the glacial chronology of Mount Timpanogos, Wasatch range, Utah. Arctic and Alpine Research, 13, 25-31.
2. Anovitz, L.M., Elam, J.M., Riciputi, L.R. and Cole, D.R. (1999): The failure of obsidian hydration dating: Sources, implications and new directions. Journal of Archaeological Science, 26, 735-752.
3. Anovitz, L.M., Elam, J.M., Riciputi, L.R. and Cole, D.R. (2004): Isothermal time-series determination of the rate of diffusion of water in Pachuca obsidian. Archaeometry, 46, 301-326.
4. Anovitz, L.M., Cole, D. and Fayek, M. (2008): Mechanisms of rhyolitic glass hydration below the glass transition. American Mineralogist, 93, 1166-1178.
5. Aoki T. (1994): Chronological study of glacial advances based on the weathering-rind thickness of morainic gravels in the northern part of the Central Japan Alps. Geographical Review of Japan, 67A, 601-618.
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