The isostatic gravity anomaly: key to the evolution of the ocean-continent boundary at passive continental margins

Details The isostatic gravity anomaly: key to the evolution of the ocean-continent boundary at passive continental margins The isostatic gravity anomaly: key to the evolution of the ocean-continent boundary at passive continental margins

May 1977

adsabs.harvard.edu/cgi-bin/nph-data_query?bibcode=1977e%26psl..35..145r&link_type=abstract

Earth and Planetary Science Letters, Volume 35, Issue 1, p. 145-150.

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Scientific paper

Isostatic gravity highs bordering the passive continental margins are interpreted as resulting from oceanic basement highs. These basement elevations are relics of the transient phenomenon of a higher ridge axis elevation during early rifting. The steep landward gradient in the isostatic gravity field, generally associated with a magnetic edge effect anomaly, delineates the boundary between oceanic and continental basement. Department of Geological Sciences, Columbia University in the City of New York, N.Y.

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