Artigo Acesso aberto Revisado por pares

Talc at fault

2007; Nature Portfolio; Volume: 448; Issue: 7155 Linguagem: Inglês

10.1038/448756a

ISSN

1476-4687

Autores

Christopher Wibberley,

Tópico(s)

High-pressure geophysics and materials

Resumo

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. High rates of creep along parts of the San Andreas fault have been attributed to low fault strength associated with serpentinized rocks. This is problematic because the frictional strength of serpentine minerals is considered too high to account for any weakness. Diane Moore and Michael Rymer now report that talc — the soft magnesium silicate mineral familiar in its pure form as talcum powder — may be behind the high creep rate. They discovered talc in serpentinite samples collected during drilling of the SAFOD (San Andreas Fault Observatory at Depth) main hole in 2005. The frictional strength of talc at elevated temperatures is sufficiently low to meet the constraints on shear strength of the fault, and its inherently stable sliding behaviour is consistent with fault creep.

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