Palaeomagnetism of the monzonite porphyry from Milton, New South Wales
作者： William A. Robertson
DOI: 10.1007/BF00880511
关键词: Geophysics 、 Quartz monzonite 、 Geology 、 Paleomagnetism 、 Divergence 、 Stability test 、 Natural remanent magnetization 、 Permian 、 Intrusion 、 Remanence 、 Paleontology
摘要: Directions of natural remanent magnetization aftermagnetic cleaning specimens from monzonite porphyry at Milton are given. Thermal and alternating magnetic field stability tests indicate that the resultant direction is earth's time cooling. Comprison pole position calculated this result with other positions rocks known age confirms probable Permian intrusion wide divergence Australian European North American age.
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