GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
Filter
  • Blackwell Publishing Ltd  (2)
  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Publishing Ltd
    Geophysical prospecting 22 (1974), S. 0 
    ISSN: 1365-2478
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences , Physics
    Notes: A set of parabolae is defined to approximate the observed gravity profile for specifying the lateral density variation in a two dimensional causative body. This variation separates the “biased” as well as “unbiased” residual anomaly structure. The method may be directly incorporated into existing numerical and graphical techniques of interpretation for subsequent delineation of structural configuration. The simple relations derived by inspection of the observed gravity profile permit universal application of the technique and in particular for the determination of the size and shape of sub-shelf structures. The suitability of the method in various problems of two dimensional interpretation has been indicated through an illustration of the Godavari Basin (India).
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
  • 2
    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: Palaeomagnetic results are presented for 95 specimens from 10 sites from the Jos Plateau Cainozoic basalts in the Northern Nigeria volcanic province. Available K–Ar age determinations from this area suggest that the rocks formed during the Pleistocene. After alternating field demagnetization, the mean direction of the natural remanent magnetization is D= 341.7°, I=–8.7° with α95= 4.2°. This yields a virtual geomagnetic pole position of 67.0°S, 63.0°E.An estimated average palaeomagnetic latitude of about 4.4°S for the area of study when compared with the present geographic latitude of about 9.5°N, implies a latitudinal northward drift of about 14° for the African plate since the time of formation of the rocks. This is incompatible with current models for plate motions and most likely represents the effects of conditional local tectonic movements or departures of the geomagnetic field from an axial dipole configuration.
    Type of Medium: Electronic Resource
    Location Call Number Limitation Availability
    BibTip Others were also interested in ...
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...