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  • 1
    Electronic Resource
    Electronic Resource
    Sea Floor Spreading as a Factor of Tectonic Evolution in Southern Chile (1969)
    [s.l.] : Nature Publishing Group
    Nature 222 (1969), S. 366-369 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] In this article I explore the possibility of a mechanism, involving sea floor spreading which agrees with the tectonics of an active continental border. New field observations in geology and geomorphology are contributed in an attempt to clarify the evolution of a little known sector of the Chilean ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/222366a0
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    Paper (German National Licenses)
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  • 2
    Electronic Resource
    Electronic Resource
    A Model for the Occurrence of Large Earthquakes (1966)
    [s.l.] : Nature Publishing Group
    Nature 211 (1966), S. 954-956 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] From these assumptions it follows that Y, the largest annual earthquake magnitude, is distributed with cumulative distribution function G(y), where G(y) = Pr = S = exp - .](.. &)]* exp (- (2) The cumulative distribution function (2) is called the "type 1" distribution of largest ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/211954b0
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  • 3
    Electronic Resource
    Electronic Resource
    Direct evidence of a subducted plate under southern Mexico (1982)
    [s.l.] : Nature Publishing Group
    Nature 296 (1982), S. 235-238 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The destructive earthquake of 24 October 1980 in the Mixtec Highlands (ML = 7.4, h = 70 km) generated over 50 aftershocks which were large enough to be recorded and located on the RESMAC telemetric network. On each record a prominent arrival is found between 10 and 20 s after the initial P signal ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/296235a0
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