A Test of Hypotheses Regarding Quartz Cementation in Sandstones: A Quantitative Image Analysis Approach
- Richard H. Worden3,
- Sadoon Morad4
Published Online: 17 MAR 2009
DOI: 10.1002/9781444304237.ch6
Copyright © 2000 The International Association of Sedimentologists
Book Title

Quartz Cementation in Sandstones
Additional Information
How to Cite
Prince, C. M. and Ehrlich, R. (2009) A Test of Hypotheses Regarding Quartz Cementation in Sandstones: A Quantitative Image Analysis Approach, in Quartz Cementation in Sandstones (eds R. H. Worden and S. Morad), Blackwell Publishing Ltd., Oxford, UK. doi: 10.1002/9781444304237.ch6
Editor Information
- 3
School of Geosciences, The Queen's University, Belfast, BT7 1NN, UK
- 4
Sedimentary Geology Research Group, Institute of Earth Sciences, Uppsala University, Norbyvägen 18 B, S–75236, Uppsala, Sweden
Publication History
- Published Online: 17 MAR 2009
- Published Print: 3 MAR 2000
ISBN Information
Print ISBN: 9780632054824
Online ISBN: 9781444304237
- Summary
- Chapter
Keywords:
- test of hypotheses regarding quartz cementation in sandstones;
- image analysis - petrographic image analysis;
- domainal porosity;
- specific perimeter - sensitive to shape complexity of porosity;
- total optical porosity;
- 2-D Fourier transform - signal analysis tool;
- well-packed/expanded ratio
Summary
Quartz cementation in sandstones is driven by the redistribution of silica. Three different processes have been proposed as having a major effect on this redistribution: (i) thermodynamic surface energy; (ii) diffusive transport; and (iii) advective transport. We have used quantitative image analysis procedures to test these hypotheses and have found all three to be lacking. Using a suite of quartz-rich sands and sandstones, as well as a suite of artificial sands made from progressively sintered glass spheres, we have found that in every case, the cementation in quartz-rich sands is a simple process that is indistinguishable from the mechanical compaction and plastic deformation found in the artificial sands.
