Interpretation of magnetic anomalies across Norfolk Ridge
- 1 November 1967
- journal article
- research article
- Published by Taylor & Francis in New Zealand Journal of Geology and Geophysics
- Vol. 10 (5) , 1302-1308
- https://doi.org/10.1080/00288306.1967.10420221
Abstract
Total magnetic force anomalies across Norfolk Ridge are caused by basaltic extrusions which are normally magnetised with an average magnetisation of 1.4 × 10−2 e.m.u. These rocks have a minimum thickness of about 1.–2.0 km in the central part of the ridge, and are covered by a thin layer of non-magnetic deposits.Keywords
This publication has 4 references indexed in Scilit:
- Structural relationships in the Tasman Sea and South-West Pacific OceanNew Zealand Journal of Geology and Geophysics, 1967
- A geophysical investigation of the Peru-Chile TrenchMarine Geology, 1966
- The Magnetic Properties of some Submarine Oceanic LavasGeophysical Journal International, 1964
- Southwest Pacific crustal structureEOS, Transactions American Geophysical Union, 1955