Articles | Volume 17, issue 2
https://doi.org/10.5194/se-17-225-2026
https://doi.org/10.5194/se-17-225-2026
Research article
 | 
06 Feb 2026
Research article |  | 06 Feb 2026

Mineralogic controls on fault displacement-height relationships

Adam J. Cawood, David A. Ferrill, Kevin J. Smart, and Michael J. Hartnett

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Cited articles

Alcalde, J., Bond, C. E., Johnson, G., Ellis, J. F., and Butler, R. W. H.: Impact of seismic image quality on fault interpretation uncertainty, GSA Today, 27, 4–10, 2017. 
Allan, U. S.: Model for hydrocarbon migration and entrapment within faulted structures, AAPG Bull., 73, 803–811, 1989. 
Aydin, A. and Basu, A.: The Schmidt hammer in rock material characterization, Eng. Geol., 81, 1–14, 2005. 
Bauer, H., Schröckenfuchs, T. C., and Decker, K.: Hydrogeological properties of fault zones in a karstified carbonate aquifer (Northern Calcareous Alps, Austria), Hydrogeol. J., 24, 1147–1170, 2016. 
Barton, C. A., Zoback, M. D., and Moos, D.: Fluid flow along potentially active faults in crystalline rock, Geology, 23, 683–686, 1995. 
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Short summary
We studied faults in Utah to understand how rock type controls fault dimensions. Using photogrammetry, field mapping, and mineral data, we found faults grow differently in weak and strong rocks because of variable mineralogy. For equivalent displacements, faults tend to be shorter in clay-rich layers and taller in rocks containing strong minerals. We built a model to predict hidden fault height from mineralogy and applied it to seismic data, showing fault dimensions are often underestimated.
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