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Krumbholz M, Hieronymus CF, Burchardt S, et al. Weibull-distributed dyke thickness reflects probabilistic character of host-rock strength. Nat Commun. 2014;5:3272doi: 10.1038/ncomms4272.
Krumbholz, M., Hieronymus, C. F., Burchardt, S., Troll, V. R., Tanner, D. C., & Friese, N. (2014). Weibull-distributed dyke thickness reflects probabilistic character of host-rock strength. Nature communications, 53272. https://doi.org/10.1038/ncomms4272
Krumbholz, Michael, et al. "Weibull-distributed dyke thickness reflects probabilistic character of host-rock strength." Nature communications vol. 5 (2014): 3272. doi: https://doi.org/10.1038/ncomms4272
Krumbholz M, Hieronymus CF, Burchardt S, Troll VR, Tanner DC, Friese N. Weibull-distributed dyke thickness reflects probabilistic character of host-rock strength. Nat Commun. 2014;5:3272. doi: 10.1038/ncomms4272. PMID: 24513695; PMCID: PMC3926007.
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Nat Commun. 2014;5:3272. doi: 10.1038/ncomms4272.

Weibull-distributed dyke thickness reflects probabilistic character of host-rock strength.

Nature communications

Michael Krumbholz, Christoph F Hieronymus, Steffi Burchardt, Valentin R Troll, David C Tanner, Nadine Friese

Affiliations

  1. 1] Department of Earth Sciences, Uppsala University, Villavägen 16, 75236 Uppsala, Sweden [2] Geoscience Center Göttingen, Georg-August Universität, Goldschmidtstraße 1-3, 37077 Göttingen, Germany [3].
  2. 1] Department of Earth Sciences, Uppsala University, Villavägen 16, 75236 Uppsala, Sweden [2].
  3. 1] Department of Earth Sciences, Uppsala University, Villavägen 16, 75236 Uppsala, Sweden [2] Geoscience Center Göttingen, Georg-August Universität, Goldschmidtstraße 1-3, 37077 Göttingen, Germany.
  4. Department of Earth Sciences, Uppsala University, Villavägen 16, 75236 Uppsala, Sweden.
  5. Leibniz Institute of Applied Geophysics, Section 1-Seismics, Gravimetry, Magnetics, Stilleweg 2, 30655 Hannover, Germany.
  6. 1] Geoscience Center Göttingen, Georg-August Universität, Goldschmidtstraße 1-3, 37077 Göttingen, Germany [2] Wintershall Norge AS, Kanalpiren, Laberget 28, 4020 Stavanger, Norway.

PMID: 24513695 PMCID: PMC3926007 DOI: 10.1038/ncomms4272

Abstract

Magmatic sheet intrusions (dykes) constitute the main form of magma transport in the Earth's crust. The size distribution of dykes is a crucial parameter that controls volcanic surface deformation and eruption rates and is required to realistically model volcano deformation for eruption forecasting. Here we present statistical analyses of 3,676 dyke thickness measurements from different tectonic settings and show that dyke thickness consistently follows the Weibull distribution. Known from materials science, power law-distributed flaws in brittle materials lead to Weibull-distributed failure stress. We therefore propose a dynamic model in which dyke thickness is determined by variable magma pressure that exploits differently sized host-rock weaknesses. The observed dyke thickness distributions are thus site-specific because rock strength, rather than magma viscosity and composition, exerts the dominant control on dyke emplacement. Fundamentally, the strength of geomaterials is scale-dependent and should be approximated by a probability distribution.

References

  1. Sci Rep. 2013 Oct 08;3:2891 - PubMed

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