Anomalous directions and paleointensity of the geomagnetic field based on paleomagnetic investigations of rocks from the Karadzha Range (Azerbaijan) of the age 45–20 ka
Paleomagnetic investigations of marine and subaqueous deposits in the 12-meter marine terrace of a section of the Karadzha Range (Azerbaijan) are performed. These deposits correspond to OI stage 3 and encompass the time interval ∼45–20 ka. Four anomalous deviations of the magnetization from the dipo...
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Veröffentlicht in: | Izvestiya. Physics of the solid earth 2009-06, Vol.45 (6), p.508-519 |
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