From a study of five hundred and forty specimens prepared from samples taken at sixty-three sites in the Pre-Cambrian Giles Complex of Central Australia it was possible to recognize a stable magnetization. The results established that the Giles Complex was in its present position at the time of acquisition of its TRM. The magnetic properties tended to correlate with the state of exsolution and oxidation of the iron-titanium oxides in the rocks.
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R. A. Facer (1971) studied this question.
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