An analysis of the variation of ocean floor bathymetry and heat flow with age¶
Parsons, B., & Sclater, J. G. (1977). An analysis of the variation of ocean floor bathymetry and heat flow with age. Journal of Geophysical Research, 60-80.
Cited by¶
1 citation across 1 artifact.
Domain-specific¶
- Isostasy
- Ocean basins and oceanic lithosphere. In marine geophysics, the systematic deepening of the seafloor with crustal age — the Parsons–Sclater age–depth relation — is isostatic: as oceanic lithosphere cools, thickens, and densifies away from the ridge, it subsides to maintain the column balance, so bathymetry encodes thermal age
SupportedVerified against the source
- Ocean basins and oceanic lithosphere. In marine geophysics, the systematic deepening of the seafloor with crustal age — the Parsons–Sclater age–depth relation — is isostatic: as oceanic lithosphere cools, thickens, and densifies away from the ridge, it subsides to maintain the column balance, so bathymetry encodes thermal age
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