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Seismology / Structural geology / Delamination / San Andreas Fault / Fault / Parkfield earthquake / Earthquake / Lithosphere / Outer trench swell / Geology / Geography of California / Plate tectonics


Geology, published online on 11 July 2013 as doi:[removed]G34244.1 Geology Lithospheric convective instability could induce creep along part of the San Andreas fault Laetitia Le Pourhiet and Jason Saleeby
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Document Date: 2013-10-07 14:38:10


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City

San Francisco / Sierra / Pasadena / Paris / Oxford / Parkfield / Loma Prieta / Sierra Nevada / San Juan / /

Company

Gre ast Co SF / /

Continent

America / /

Country

France / United States / United Kingdom / /

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Event

Natural Disaster / /

Facility

Andreas Fault Observatory / Fort Tejon / San Andreas Fault Observatory / Tectonics Observatory / California Institute of Technology / Sierran basement / /

IndustryTerm

online articles / energy / Advance online articles / seismic imaging data / gravitational potential energy / /

MusicAlbum

Production / /

NaturalFeature

Great Valley / Death Valley / Eastern Sierra / Sierra Nevada Mountains / Sierra Nevada / /

Organization

Betty Moore Foundation / California Institute of Technology / Division of Earth and Planetary Sciences / Seismological Society of America Bulletin / U.S. government / Geological Society of America Bulletin / Division of Earth / Institut National / American Association of Petroleum Geologists Bulletin / Geological Society of America Geology / INSU / General Services Administration / Division of Geological and Planetary Science / /

Person

Morgan Hill / Laetitia Le Pourhiet / Jason Saleeby Geology / /

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ProvinceOrState

Nevada / California / New Hampshire / /

PublishedMedium

Geophysical Research Letters / Journal of Geophysical Research / /

Region

northern California / central California / /

Technology

3-D / GPS / v. 22 / Geophysics / v. 32 / http / digital object identifier / /

URL

www.gsapubs.org/subscriptions / www.gsapubs.org/cgi/alerts / www.gsapubs.org / www.geosociety.org/pubs/copyrt.htm#gsa / /

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