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  • 1
    Call number: 5/M 01.0188 ; 5/M 01.0188(2.Ex.)
    In: Geophysical monograph
    Type of Medium: Monograph available for loan
    Pages: viii, 398 Seiten , Illustrationen
    ISBN: 0-87590-979-5
    Series Statement: Geophysical monograph 121
    Language: English
    Location: Reading room
    Location: Reading room
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 2
    Electronic Resource
    Electronic Resource
    Palo Alto, Calif. : Annual Reviews
    Annual Review of Earth and Planetary Sciences 26 (1998), S. 615-642 
    ISSN: 0084-6597
    Source: Annual Reviews Electronic Back Volume Collection 1932-2001ff
    Topics: Geosciences , Physics
    Notes: Abstract The central assumption of plate tectonics, that plate interiors are rigid, remains a useful but uncertain approximation. Strain rates of stable plate interiors are bounded between 10-12-10-11 year-1 and ~4 x 10-10 year-1. The narrowness of all plate boundaries, the other main assumption of plate tectonics as originally conceived, is contradicted by many observations, both in the continents and in the oceans. Some diffuse plate boundaries in both continents and oceans exceed dimensions of 1000 km on a side. Diffuse plate boundaries cover ~15% of Earth's surface. The maximum speed of relative plate motion across any one diffuse plate boundary ranges from ~2 to ~15 mm/year, which is faster than some upper bounds on intraplate motion across stable plate interiors (〈=2 mm year-1). Strain rates in diffuse plate boundaries can be as high as ~10-8 year-1, ~25 times higher than the upper bound on strain rates of stable plate interiors, but ~600 times lower than the lowest strain rates across typical narrow plate boundaries. The poles of rotation of the plates flanking a diffuse oceanic plate boundary tend to be located in the diffuse boundary, which is a consequence of the strong coupling across the boundary.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillan Magazines Ltd.
    Nature 404 (2000), S. 139-140 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] Today, Antarctica seems to be part of a single tectonic plate. But there is clear palaeomagnetic evidence that, in the past, there has been a large relative rotation between different parts of the continent. A central issue has been how much, if any, of this motion has occurred during the past ...
    Type of Medium: Electronic Resource
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  • 4
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 387 (1997), S. 131-133 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] True polar wander is the slow, secular shift of the entire solid Earth, relative to its rotation axis, in response to Earth's changing distribution of mass. In recent years the emphasis of dynamical models for true polar wander has turned from deglaciation, which is responsible for much of the ...
    Type of Medium: Electronic Resource
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  • 5
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 106 (1991), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We use the skewness of seafloor-spreading magnetic anomalies 27r–31 to determine a revised Late Maastrichtian–early Palaeocene palaeomagnetic pole for the Pacific plate. We used numerical experiments to estimate the potential information in magnetic profiles that had not been previously analysed for skewness information. The results indicated that profiles obtained between the Murray and Galapagos fracture zones would be the most useful because in this region very different values of remanent magnetic effective inclination are predicted for small changes in the assumed palaeomagnetic pole position. Furthermore, these data would constrain the pole in the direction most poorly constrained by prior data. Using 50 skewness estimates from 17 profiles, we compute a well-constrained pole that agrees with a pole computed from other types of data with similar ages. These other data include a seamount palaeomagnetic pole, effective inclinations from two submarine ridges, palaeolatitudes determined from azimuthally unoriented cores of submarine basalt and from a piston core in deep-sea sediments, two palaeo-equators from equatorial sediment facies, and amplitude data from magnetic lineations. Combining all the data, we determine a best-fit 65 Ma palaeomagnetic pole for the Pacific plate that is located at 71.6°N, 7.9°E. The 95 per cent confidence ellipse for the new pole, a 2.9° major semiaxis oriented 75° clockwise of north and a 1.8° minor semiaxis, is ∼50 per cent smaller in area than that for the prior pole. We conclude that anomaly skewnesses can be used to determine accurate palaeomagnetic poles for plates containing oceanic lithosphere.
    Type of Medium: Electronic Resource
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  • 6
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 118 (1994), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: An increase in the accuracy and age resolution of the apparent polar wander path of the Pacific plate could be important for testing reconstructions that relate the motion of Pacific basin plates to other plates, for testing if hotspots in different ocean basins are stationary relative to one another, and for estimating the motion of hotspots relative to the spin axis. With these goals in mind, herein we investigate how accurately a palaeomagnetic pole can be estimated from skewness analysis of many crossings of a single magnetic anomaly on the Pacific plate. Apparent effective remanent inclinations of the sea-floor magnetization were estimated from the skewnesses of 132 useful (out of 149 total) crossings of anomaly 25r (56.5–57.8 Ma) distributed over a distance of more than 11000 km across the Pacific plate. These estimates were inverted to obtain a best-fitting palaeomagnetic pole latitude, pole longitude, and anomalous skewness for this single reversed-polarity chron. The best-fitting model gives a pole of 78.2°N, 4.8°E with a 95 per cent confidence ellipse having a 6.4° major semi-axis oriented 93° clockwise of north and a 4.1° minor semi-axis; anomalous skewness is 16.2°± 4.6° (95 per cent confidence limits). We also investigated the effect of the dependence of anomalous skewness on spreading rate by correcting our data using an empirical model. The pole obtained from the inversion of this alternative data set lies a statistically insignificant 0.6° from the pole obtained using no correction. That a pole with usefully compact confidence limits and a narrowly resolved, precisely estimated age can be so determined suggests that an accurate apparent polar wander path with a fine-age resolution can be determined for the Pacific plate by applying the same approach to the shapes of other marine magnetic anomalies.Comparison of our chron 25r pole with other Pacific palaeomagnetic and palaeoequatorial sediment facies data indicates that the Pacific plate remained nearly stationary relative to the spin axis during the Eocene (-0.05°Myr−1± 0.28° Myr−1), but probably moved rapidly northward during the Paleocene (0.83° Myr−1± 0.46° Myr−1). Comparison of these data to latitudes of dated volcanic edifices along the Hawaiian-Emperor chain indicates that the Hawaiian hotspot drifted southward by 10.2°± 3.4° (95 per cent confidence limits) since 57 Ma, but only by 1.7°± 1.9° since 39 Ma, which gives a southward displacement of 8.5°± 3.9° (95 per cent confidence limits) between 57 and 39 Ma, corresponding to a rate of southward motion of 52°24mm yr−1. Incorporation of realistic uncertainties of volcano ages would increase these uncertainties considerably, however. We also examined the distance between the crossings of anomalies 25 and 27 on all the profiles we analysed; along the palaeo-Pacific-Farallon boundary these distances are inconsistent with the joint hypotheses of symmetric spreading and single Pacific and Farallon plates between 62 and 56 Ma, indicating that the evidence for a single Pacific plate in early Tertiary time is not as compelling as it had previously seemed.
    Type of Medium: Electronic Resource
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  • 7
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Prior studies have proposed and examined the hypothesis that India and Australia are separate rigid plates separated by a wide, near-equatorial, E-W striking, plate boundary. Attempts to place narrow limits on the location of the Africa-Australia-India triple junction have been hindered, however, by the lack of useful magnetic profiles crossing the eastern Carlsberg Ridge and northern Central Indian Ridge. Herein we present near-ridge portions of new profiles from an aeromagnetic survey of the Carlsberg Ridge east of 66°E and of the Central Indian Ridge north of 19°S. These new data are used to estimate 35 new spreading rates averaged from the middle of chron 2A (3.03 Ma) to the present. All other plate motion data along the Central Indian and Carlsberg ridges are also analysed to investigate the present kinematics of the Indian Ocean, especially the motion and boundary between the Indian and Australian plates. Unlike prior efforts, we objectively estimate uncertainties in the strikes of transform faults along the Carlsberg and Central Indian ridges.Indian Ocean plate motion data are unambiguously inconsistent with a model in which India and Australia lie on the same rigid plate, but remain consistent with the existence of distinct and rigid Indian and Australian plates. the plate motion data also remain consistent with closure of the Africa-Arabia-India plate motion circuit. the data are consistent with closure of the Africa-Antarctic-Australia plate motion circuit and place an upper bound of 7 mm yr−1 on the summed deformation around the Rodriguez triple junction if we have accurately estimated the errors in the data. From data along the Carlsberg and Central Indian Ridges, 95 per cent confidence limits on the location of the Africa-Australia-India triple junction are 6.2°S to ∼9°S if the boundary between India and Australia is discrete (i.e. very narrow) where it intersects the Central Indian Ridge. When closure is enforced about the Owen and Rodriguez triple junctions, these limits decrease to 8°S-9°S, which is centred on the Vema fracture zone and is more than 10 times narrower than we found without the new data. the resulting specific prediction of the location of, and velocity across, a hypothetical narrow boundary between the Indian and Australian plates permits us to test the hypothesis of a narrow boundary. Available data suggest, but do not prove, that no such narrow boundary accommodating the predicted direction of
    Type of Medium: Electronic Resource
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  • 8
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical journal international 109 (1992), S. 0 
    ISSN: 1365-246X
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: We present a method for simultaneously determining palaeomagnetic poles and anomalous skewness from the observed skewness of marine magnetic anomalies from a single plate. Skewness is esimated by visual comparison of phase-shifted observed anomaly profiles with an ideal zero-phase synthetic anomaly calculated for sea-floor formed and observed in a vertical magnetic field. We assume that each crossing of the same anomaly or anomalies is anomalously skewed by an identical amount. This assumption is supported by the great reduction in squared error (i.e.,x2) obtained by adding just this one adjustable parameter. Our inversion procedure determines the palaeomagnetic pole and anomalous skewness that give a maximum likelihood best fit in a least-squares sense to the observed effective remanent inclinations, which are inferred by simple calculation from the observed phase shift. Our method determines 95 per cent confidence limits both from a constant-chi-square boundary and by linear propagation of errors and also estimates the information distribution of the data. The anomalous skewness values we determine agree with values estimated from comparison of anomalies across a spreading centre. These encouraging results suggest that further skewness studies may permit variations in anomalous skewness with age to be quantified, provide constraints for models that describe the processes affecting the magnetic source layer during its creation and evolution, and permit oceanic plate apparent polar wander paths to be determined with a fine age resolution.
    Type of Medium: Electronic Resource
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  • 9
    Electronic Resource
    Electronic Resource
    [s.l.] : Macmillan Magazines Ltd.
    Nature 398 (1999), S. 64-67 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] The East African rift marks the northern boundary of the Nubian (West African) and Somalian (East African) plates, and has formed by horizontal stretching due to the separation of these plates. South of ∼20° S, any expression of deformation or seismicity due to the relative ...
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature 364 (1993), S. 760-761 
    ISSN: 1476-4687
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Chemistry and Pharmacology , Medicine , Natural Sciences in General , Physics
    Notes: [Auszug] ARE the Earth's plate motions steady, or do they change over millions of years, hundreds of thousands of years, or shorter intervals? The motion of some plates has been nearly constant over the past 5 million years, according to Douglas Wilson, whose results are reported on page 788 ...
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