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- W2084394501 abstract "An extensive collection of palaeomagnetic samples of Upper Permian and Lowet Triassic rocks has been accumulated in the region of the Czechoslovakian western Carpathian Mountains. The original objective was to attempt an empirical correlation of rocks on the basis of normally and reversely magnetized zones, or to define rocks with reverse magnetization which could belong to the Permian if this period were to be characterized solely by reverse magnetization. This paper points out some hitherto unclarified global aspects and endeavours to solve such a problem; the boundary between the Permian and the Triassic has not yet been determined by using palaeomagnetism. On the other hand, abundant statistical palaeomagnetic material is available which data can be interpreted in relation to the rotational effect of Alpine tectonics. In these preliminary results systematic deviations of palaeomagnetic declination in samples from the Choč nappe could be discerned, and they are considered to be the result of Alpine tectonic movements of rotational character. This geophysical interpretation confirms the geological concept of overthrust structure for the western Carpathian region. In conclusion a brief mention is made about the fact that, even during global interpretation of palaeomagnetic pole positions, the possible effect of horizontal rotational movements of entire rock blocks should be taken into consideration. This is of special importance in regions of high tectonic mobility, and must be taken into account in explaining the differences in pole positions viewed from different continents (e.g., in connection with continental drift)." @default.
- W2084394501 created "2016-06-24" @default.
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- W2084394501 date "1965-01-01" @default.
- W2084394501 modified "2023-09-23" @default.
- W2084394501 title "Palaeomagnetic study of tectonic rotation in the Carpathian mountains of Czechoslovakia" @default.
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- W2084394501 doi "https://doi.org/10.1016/0031-0182(65)90005-2" @default.
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