Precambrian Cratons

In the 1960s and 1970s there was considerable interest in Archean and Proterozoic paleomagnetism, and studies were made in all the major cratons of the present continents. The general method of presentation of these studies was to allow the paleomagnetic poles to fall within an APWP swathe of -20 width. These swathes were then drawn so as to incorporate all the pole positions by making suitable bends and curves in the swathe where necessary. As a result of this approach Piper et al. (1973)...

Table

High-Temperature (Deuteric) Oxidation Classification Scheme from Wilson and Watkins (1967) I Homogeneous (single-phase) titanomagnetites II Titanomagnetites contain a few exsolved ilmenite lamellae in 111 planes III Abundant ilmenite lamellae with equilibrium two-phase intergrowths IV Ilmenite lamellae oxidized to rutile + hematite V Residual titanomagnetite and ilmenite oxidized to rutile + hematite VI Total oxidation to pseudobrookite and hematite and or rutile A useful empirical...

The Geomagnetic Polarity Time Scale

4.2.1 Polarity Dating of Lava Flows 0-6 Ma Mercanton (1926) first realized that if rocks containing reverse magnetizations were due to reversals of the Earth's magnetic field, then this should be registered in rocks worldwide and so he obtained samples from Spitsbergen, Greenland, Iceland, the Faroe Islands, Mull, Jan Mayen Land and Australia as a test. He found that some were magnetized in the same sense as the present Earth's field and others were roughly reversed from it. Matuyama (1929)...

Non Plate Tectonic Hypotheses

In paleomagnetism it is important to distinguish between the concepts of polar wandering and continental drift. All measurements in paleomagnetism are made with respect to the geographic pole as the frame of reference. Therefore, in plate tectonics the concept of polar wander may appear to be meaningless because all one is saying is that the reference frame itself is in motion. True polar wander, TPW, on the other hand, has been defined as the displacement of the entire Earth with respect to...

Modeling Marine Magnetic Anomalies

5.2.1 Factors Affecting the Shape of Anomalies The anomalies expected from the Vine-Matthews crustal model will vary depending on location and age. Consider the case of symmetrical anomalies about a spreading ridge at the north pole and about N-S or E-W oriented ridges at the equator as shown in Fig. 5.10. The crustal blocks will be magnetized in opposite directions as the polarity changes, but only the first magnetic reversal is

Field Tests for Stability

3.3.1 Constraining the Age of Magnetization In favorable circumstances it is possible to arrange paleomagnetic sampling so that field tests can be performed to constrain the age of magnetization. Graham 1949 proposed two such tests referred to as the fold test and the conglomerate test. Later, Everitt and Clegg 1962 introduced the baked contact test. The circumstances for each of these tests are illustrated in Fig. 3.4. More recently Kirschvink 1978 proposed the unconformity test, which is only...

S

Methods for determining the Earth's paleoradius. a The paleomeridian method of Egyed 1960 . Cross-section through the Earth with two sampling sites S, and S2 lying on a paleomeridian separated by distance d. If their paleolatitudes are gt ., and .2, the ancient radius a is determined from 7.1.13 . b The minimum dispersion method of Ward 1963 . The positions of rock units X , lt j gt are transformed to a new co-ordinate system using the center of the continent as the pole center of...

Info

Variations of the dipole field with time since A.D. 1600. a Variation of the dipole moment from successive spherical harmonic analyses, b Variation of the dipole axis as represented by the change in position of North Geomagnetic Pole. After Fraser-Smith 1987 . speculated on the demise of the main dipole around A.D. 3700 to 4000 if the present trends continue, but this change is probably just part of the natural variation as the dipole recovers from abnormally high values at about 2000...