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  • 1
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Reversals of the Earth's magnetic field reflect changes in the geodynamo—flow within the outer core—that generates the field. Constraining core processes or mantle properties that induce or modulate reversals requires knowing the timing and morphology of field changes that ...
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  • 2
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillian Magazines Ltd.
    Nature 401 (1999), S. 885-890 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] A series of computer simulations of the Earth's dynamo illustrates how the thermal structure of the lowermost mantle might affect convection and magnetic-field generation in the fluid core. Eight different patterns of heat flux from the core to the mantle are imposed over the core–mantle ...
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 123 (1995), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We present a new palaeomagnetic investigation of the two sites from the Steens Mountain (Oregon) volcanic record of a Miocene polarity reversal which were supposed to record very fast changes of the geomagnetic field or impulses (Mankinen et al. 1985; Prévot et al. 1985a,b). Approximately 130 cores were first drilled from the two initial sites, belonging to sections A and B, in order to obtain at least one detailed and complete vertical sampling of each lava flow. Thermal analyses of natural remanent magnetization, complemented by some alternating field treatments, low-field thermo-magnetic curves, microscopic observations and electron probe analyses of key magnetic phases, lead us to somewhat different conclusions for the first and the second impulses. At site B (first impulse), we find that the dependence of the remanence direction on the sample vertical position in flow B51 does not imply a directional field change during flow cooling, but is better explained by a thermochemical overprinting due to the overlying B50 flow. However, this conclusion does not challenge the existence of the first impulse because this field change seems to be recorded some 25 m away in flow B51 (Coe & Prévot 1989), at a place where it is thick enough for this record not to have been erased by the baking due to B50. Regarding the second impulse, restudied at site A, our new findings are more comprehensively explained by a change in the field direction during cooling of flow A41–2 than by some overprinting. Using a simple model of flow cooling, the angular rate of change of the field is estimated to have been of the order of 2°-3° or 250–350 nT per day during the impulse. This figure is similar to that previously obtained from site D, some 250 m away. However, the directional paths describing the field change are somewhat different at the two sites. New investigations are planned to try to understand the origin of this discrepancy.
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  • 4
    Electronic Resource
    Electronic Resource
    Springer
    Contributions to mineralogy and petrology 26 (1970), S. 247-264 
    ISSN: 1432-0967
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract The transition of orthoenstatite to clinoenstatite which has been observed experimentally under conditions of nonhydrostatic stress by many workers is interpreted to be a coherent polymorphic transition involving a transformation strain of simple finite shear. Depending on whether the angle of shear is 13.3 or 18.3°, thermodynamic treatment predicts that the transition temperature is raised 177 or 248° C respectively per kilobar of shear stress on (100) parallel to [001] if the change of entropy is arbitrarily assumed to be 1 cal/° C-mole. The rareness with which clinoenstatite is found in naturally deformed terrestrial rocks containing orthoenstatite may mean that shear stresses are rarely large enough in nature to cross the thermodynamic phase boundary. The orthoferrosilite-clinoferrosilite and parawollastonite-wollastonite transitions are thought to be analogous, and similarly large thermodynamic effects of shear stress are predicted.
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  • 5
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 311 (1984), S. 684-684 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] K.M. Crer and his co-editors frankly confess to holding "mixed views about the publication of symposium proceedings". Such pessimism was misplaced; to my mind, they have succeeded admirably in avoiding the pitfalls that doom most books of this genre to a limited readership and transient life. ...
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  • 6
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 316 (1985), S. 230-234 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] A highly detailed record of both the direction and intensity of the Earth's magnetic field as it reverses has been obtained from a Miocene volcanic sequence. The transitional field is low in intensity and is typically non-axisymmetric. Geomagnetic impulses corresponding to astonishingly high ...
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  • 7
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 327 (1987), S. 141-144 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Most palaeomagnetic data of Permian age for the SCB are derived from the Emeishan Basalt Formation, which is widespread throughout south-west China. In 1980 one of us (X.Z.) sampled 32 lava flows spanning 212m of section at the type locality (29.6° N, 103.4° E) on the east limb of the Nubeishan ...
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  • 8
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 362 (1993), S. 51-53 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Many papers5'7'9 discuss the statistical validity of the observational evidence for persistent transition paths. Here we discuss a different aspect of the problem: their possible underlying cause. One of us (D.G.) developed the model described below10 before it was explained to him by the second ...
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  • 9
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 367 (1994), S. 57-59 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Mono Basin (Fig. 1) has proved to be an almost ideal natural laboratory in which to study the fidelity of sedimentary magnetization. Well-exposed sections outcrop in several places around the lake and contain numerous tephra marker horizons that enable unambiguous identification of stratigraphic ...
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 295 (1982), S. 399-401 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Two simple models of the reversing field have been proposed in the past 5 years3'4. The two involve conceptually different source mechanisms and, in their purest forms, make distinct predictions of transitional field behaviour. Although it is possible that no single process controls transitional ...
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