Systematics of paleomagnetic directions from early–middle Devonian rocks of Minusa troughs: new data and old problems

作者: A. V. Shatsillo , V. E. Pavlov

DOI: 10.1134/S1069351319030091

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摘要: Paleomagnetic results from numerous Early–Middle Devonian volcanic sequences of the Minusa trough, southern Siberia, are presented. The analysis these data definitely indicates that geomagnetic field in had a specific character, different both present and more ancient geological epochs, was extremely variable (hyperactive). anomalies paleomagnetic record not local, peculiar to particular region, but have global occurrence. synthesis obtained with coeval volcanics Scotland shows during relatively short time (10–20 Ma), pole repeatedly changed its location, significantly deviating Earth’s rotation axis up (paleo)equator assuming some quasi-stable positions. arguments suggesting features could probably be induced by significant contribution equatorial dipole main

参考文章(23)
A. N. Khramov, A. G. Iosifidi, Asymmetry of geomagnetic polarity: Equatorial dipole, Pangaea, and the Earth’s core Izvestiya-physics of The Solid Earth. ,vol. 48, pp. 28- 41 ,(2012) , 10.1134/S1069351312010077
J. T. Sallomy, J. D. A. Piper, Palaeomagnetic Studies in the British Caledonides?IV Lower Devonian Lavas of the Strathmore Region, Scotland Geophysical Journal International. ,vol. 34, pp. 47- 68 ,(1973) , 10.1111/J.1365-246X.1973.TB02385.X
A. N. Khramov, Geomagnetic reversals in the paleozoic: A transitional field, polarity bias, and mantle convection Izvestiya-physics of The Solid Earth. ,vol. 43, pp. 800- 810 ,(2007) , 10.1134/S1069351307100023
Geoffrey S Watson, Randolph J Enkin, None, The fold test in paleomagnetism as a parameter estimation problem Geophysical Research Letters. ,vol. 20, pp. 2135- 2137 ,(1993) , 10.1029/93GL01901