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| Ship Operations >> Schedules >> Melville >> Index >> Project Description >> |
| Project Description |
The geophysical data (multibeam bathymetric, 3.5 KHz, magnetic and gravity) will be used to document the character of short wavelength magnetic anomalies within the Cretaceous Quiet Zone (KQZ; 83-120.6 Ma), an approximately 38 million year long interval of constant normal polarity of the geomagnetic field. Since lineated short wavelength magnetic anomalies, attributed to paleointensity fluctuations and short polarity events, have been documented over oceanic crust both older and younger than the KQZ, our expectation is that coherent lineations of geomagnetic origin will also be present in our proposed study area (a region of ultra-fast spreading in the southwestern Pacific). Such coherent features can be used as time markers for tectonic studies within this 38 m.y. interval. If no such correlatable features are found we will have established a major difference between geomagnetic field behavior in the KQZ and at other times. In either case, the character of the non-lineated anomalies together with multibeam bathymetry will provide information on crustal heterogeneity at this ultrafast spreading ridge.
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