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Rinded iron-oxide concretions: hallmarks of altered siderite masses of both early and late diagenetic origin

  1. DAVID B. LOOPE1,
  2. RICHARD M. KETTLER1,
  3. KARRIE A. WEBER1,2,
  4. NATHAN L. HINRICHS1,
  5. DEREK T. BURGESS1

Article first published online: 12 MAR 2012

DOI: 10.1111/j.1365-3091.2012.01325.x

Issue

Sedimentology

Sedimentology

Volume 59, Issue 6, pages 1769–1781, October 2012

Additional Information

How to Cite

LOOPE, D. B., KETTLER, R. M., WEBER, K. A., HINRICHS, N. L. and BURGESS, D. T. (2012), Rinded iron-oxide concretions: hallmarks of altered siderite masses of both early and late diagenetic origin. Sedimentology, 59: 1769–1781. doi: 10.1111/j.1365-3091.2012.01325.x

Author Information

  1. 1

    Department of Earth & Atmospheric Sciences, University of Nebraska, Lincoln, NE 68588-0340, USA (E-mail: dloope1@unl.edu)

  2. 2

    School of Biological Sciences, University of Nebraska, Lincoln, NE 68588-0118, USA Associate Editor – Peter Talling

Publication History

  1. Issue published online: 18 SEP 2012
  2. Article first published online: 12 MAR 2012
  3. Accepted manuscript online: 3 FEB 2012 11:53AM EST
  4. Manuscript received 9 April 2011; revision accepted 3 January 2012

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