Magnetic anomalies across Campbell Plateau,New Zealand |
| |
| Authors: | FJ Davey DA Christoffel |
| |
| Institution: | Geophysics Division, Department of Scientific and Industrial Research, Wellington New Zealand;Physics Department, Victoria University of Wellington, Wellington New Zealand |
| |
| Abstract: | 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. |
| |
| Keywords: | |
| 本文献已被 ScienceDirect 等数据库收录！ |
|
