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• W848455427 abstract "statistically significant number of samples and sites, can give a reliable record of the ancient geomagnetic field at the site of rock formation. The basic hypothesis that the geomagnetic field was, on average, that of an axial and geocentric dipole permits the paleomagnetist to interpret his results in terms of paleolatitude of the sampling site and its location with respect to the paleomeridians. When paleomagnetic directions from a possibly displaced or rotated block are compared with those from a neighbouring craton, the declination difference between an expected or reference direction and an observed direction indicate the amount of rotation, whereas the paleolatitude difference indicates north-south displacement. Paleomagnetic data provide the best, often the only, means for measuring rotations on vertical axes (e.g. Jackson and McKenzie, 1989; Garfunkel, 1989). Physical and mathematical arguments show that the observed movement on faults within a wide zone of continental deformation does not in general determine the rotation rate of the rigid block bounded by faults. Only if an a priori model for the deformation is assumed can the fault movements be related to observations of paleomagnetic rotations. Even when such a model is valid, the faulting determines the block rotations relative to the boundaries of the zone, whereas the paleomagnetic data measure the rotation with respect to the Earth's rotation axis. Since geological, geodetic, seismic, and paleomagnetic measurements tend to sample complementary aspects of the deformation field, we need an integrated observation program to find the answer at the question whether deformation of continents is more accurately describe by the motion of a few small rigid plates or by quasi-continuous flow. In this paper, I will review the most important paleomagnetic results from the Romania territory. Then a discussion of paleomagnetic constrains on the Cainozoic geodynamic history will follow. The paleomagnetic data will be presented together with a review of the geological structural data (Maţenco, 1997) to support a future integrated model of tectonic evolution of Carpatho- Pannonian area." @default.
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• W848455427 date "1998-01-01" @default.
• W848455427 modified "2023-09-24" @default.
• W848455427 title "Paleomagnetic constraints of the geodynamic history of Romania" @default.
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