GEOMAGNETIC PALEOINTENSITY EXPERIMENT ON IGNEOUS AND METAMORPHIC ROCKS FROM ENDERBY LAND IN NAPIER COMPLEX, ANTARCTICA
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The modified Thelliers' and Shaw's methods are applied to granulite and igneous rocks from Mt. Riiser-Larsen in Enderby Land, some of which were dated by the K-Ar method to be of 1.2-1.4Ga. Very low paleointensities are suggested from high temperature components of the Thelliers-type results and from the Shaw-type experiment.
- 国立極地研究所の論文
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関連論文
- K-Ar AGES OF IGNEOUS AND METAMORPHIC ROCKS FROM MCMURDO, S∅R RONDANE AND DUMONT D'URVILLE, ANTARCTICA
- A preliminary study of secondary magnetization during successive heating of rocks from the Napier Complex
- PRELIMINARY NOTE ON PALEOINTENSITIES OF THE GEOMAGNETIC FIELD OBTAINED FROM ROCKS IN ANTARCTICA
- GEOMAGNETIC PALEOINTENSITY EXPERIMENT ON IGNEOUS AND METAMORPHIC ROCKS FROM ENDERBY LAND IN NAPIER COMPLEX, ANTARCTICA