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  • 1
    Electronic Resource
    Electronic Resource
    Elevation of Mid-ocean Ridges and the Evolution of the South-west Indian Ridge (1971)
    [s.l.] : Nature Publishing Group
    Nature 230 (1971), S. 175-177 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] In many regions of the ocean floor, the magnetic anomaly patterns are not nearly as distinctive. Thus, north-south trending ridges near the magnetic equator will produce magnetic anomaly patterns of low amplitude which are indistinguishable from magnetic noise. Jumps in the position of a spreading ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/230175a0
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    Paper (German National Licenses)
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  • 2
    Electronic Resource
    Electronic Resource
    Earth science Ins and outs on the ocean floor (2003)
    [s.l.] : Nature Publishing Group
    Nature 421 (2003), S. 590-591 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Earth loses internal heat in two main ways: in cooling of the ocean lithosphere, originally generated at mid-ocean ridges, and in conduction across the boundary between the mantle and the continental and oceanic lithospheres. Heat exchange between the lithosphere and the oceans then occurs through ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/421590a
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  • 3
    Electronic Resource
    Electronic Resource
    Palaeolatitudes from JOIDES Deep Sea Sediment Cores (1970)
    [s.l.] : Nature Publishing Group
    Nature 226 (1970), S. 934-935 
    Details
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Palaeomagnetic measurements of deep sea sediment cores could yield additional information about the past motions of the sea floor. Because of their short length of less than 20 m, however, these cores have been studied principally to determine the frequency and pattern of reversals in the Earth's ...
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1038/226934a0
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