Magnetic anomalies across Campbell Plateau, New Zealand

Details Magnetic anomalies across Campbell Plateau, New Zealand Magnetic anomalies across Campbell Plateau, New Zealand

Sep 1978

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1978e%26psl..41...14d&link_type=abstract

Earth and Planetary Science Letters, Volume 41, Issue 1, p. 14-20.

Physics

3

Scientific paper

Magnetic measurements over the Campbell Plateau, New Zealand, show the existence of a linear positive anomaly belt which extends for 900 km along an approximately east-west trend. This anomaly belt is considered to be a continuation of the Stokes Magnetic Anomaly occurring through New Zealand and associated with rocks of the New Zealand Geosyncline. If this is so, a transcurrent fault with a dextral displacement of about 330 km and aligned in a northeast-southwest direction must occur between the eastern end of the Stokes Magnetic Anomaly and the western end of the anomaly belt across Campbell Plateau.

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