D/H Ratios of Supergene Alunite as an Indicator of Paleoclimate in Continental Settings

  1. P. K. Swart,
  2. K. C. Lohmann,
  3. J. Mckenzie and
  4. S. Savin
  1. Greg B. Arehart and
  2. James R. O'Neil

Published Online: 2 APR 2013

DOI: 10.1029/GM078p0277

Climate Change in Continental Isotopic Records

Climate Change in Continental Isotopic Records

How to Cite

Arehart, G. B. and O'Neil, J. R. (1993) D/H Ratios of Supergene Alunite as an Indicator of Paleoclimate in Continental Settings, in Climate Change in Continental Isotopic Records (eds P. K. Swart, K. C. Lohmann, J. Mckenzie and S. Savin), American Geophysical Union, Washington, D. C.. doi: 10.1029/GM078p0277

Author Information

  1. Department of Geological Sciences, University of Michigan, Ann Arbor, MI 48109-1063

Publication History

  1. Published Online: 2 APR 2013
  2. Published Print: 1 JAN 1993

ISBN Information

Print ISBN: 9780875900377

Online ISBN: 9781118664025

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Keywords:

  • Climate changes;
  • Paleoclimatology;
  • Isotope geology;
  • Radioactive tracers

Summary

This chapter contains sections titled:

  • Introduction

  • Environments of Formation of Alunite

  • Analytical Techniques

  • Changes In δD of Alunite With Time

  • Possible Causes of Changes in δD

  • Correlation With Other Paleoclimatological Indicators

  • Summary