Is the oceanic crust over 1 km necessary for the source of marine magnetic anomalies?

Details Is the oceanic crust over 1 km necessary for the source of marine magnetic anomalies? Is the oceanic crust over 1 km necessary for the source of marine magnetic anomalies?

Nov 1987

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1987pepi...49..117f&link_type=abstract

Physics of the Earth and Planetary Interiors, Volume 49, Issue 1-2, p. 117-120.

Physics

3

Scientific paper

A paleomagnetic vertical profile over 1 km through the oceanic crust is constructed by magnetic properties of 256 DSDP samples from Hole 504B, the Costa Rica Rift. The results of magnetic measurements of the relatively young oceanic crust indicate that the thickness of the marine magnetic source layer is a 0.6 km thick pillow lava layer of the uppermost oceanic crust.

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