Gravity and magnetic anomalies over the Derwent-Hunter Guyot, Tasman Sea
- 1 March 1970
- journal article
- research article
- Published by Taylor & Francis in New Zealand Journal of Geology and Geophysics
- Vol. 13 (1) , 117-125
- https://doi.org/10.1080/00288306.1970.10428208
Abstract
Gravity and magnetic measurements from two profiles across the Derwent-Hunter Guyot in the Tasman Sea indicate that the volcanic core of the guyot is probably capped by vesicular volcanic rocks, and that the flanks are covered with a layer of sediments up to 2 – 5 km thick.Keywords
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