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Seismology

Talc at fault

Nature volume 448, pages 756–757 (2007)Cite this article

The behaviour of the San Andreas fault varies along its length — it slips in some places and creeps in others. The discovery of the ultrasoft mineral talc in rocks from deep inside the fault could help to explain why.

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Figure 1: In search of weak creep.

USGS

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Authors and Affiliations

  1. Christopher Wibberley is at the Laboratoire de Géosciences Azur, Université de Nice Sophia Antipolis, France. (In October 2007 he will move to TOTAL Centre Scientifique et Technique Jean Feger, Avenue Larribau, F-64018 Pau Cedex, France.) wibbs@geoazur.unice.fr (christopher.wibberley@total.com),

    Christopher Wibberley

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Wibberley, C. Talc at fault. Nature 448, 756–757 (2007). https://doi.org/10.1038/448756a

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