A correction for sediment load upon the ocean floor: Uniform versus varying sediment density estimations—Implications for isostatic correction
TJS Sykes - Marine Geology, 1996 - Elsevier
The isostatic correction for the sediment load on oceanic basement has often been
calculated using a uniform sediment density, irrespective of either water depth or total …
calculated using a uniform sediment density, irrespective of either water depth or total …
Southern hemisphere Miocene bottom-water circulation: a palaeobathymetric analysis
TJS Sykes, ATS Ramsay, RB Kidd - Geological Society, London …, 1998 - lyellcollection.org
Palaeobathymetric reconstructions of the southern hemisphere are used to assess the
potential flow paths and extent of proto-Antarctic Bottom Water (proto-AABW) for three time …
potential flow paths and extent of proto-Antarctic Bottom Water (proto-AABW) for three time …
Southern hemisphere palaeobathymetry
TJS Sykes, JY Royer, ATS Ramsay… - … Society, London, Special …, 1998 - lyellcollection.org
Digital grids, with a spatial resolution of 0.5°, were compiled using bathymetry, sediment
thickness and oceanic crustal ages for the southern hemisphere to calculate sediment-free …
thickness and oceanic crustal ages for the southern hemisphere to calculate sediment-free …
Thermal regime of the Southeast Indian Ridge between 88 E and 140 E: Remarks on the subsidence of the ridge flanks
The flanks of the Southeast Indian Ridge are characterized by anomalously low subsidence
rates for the 0–25 Ma period: less than 300 m Ma− 1/2 between 101° E and 120° E and less …
rates for the 0–25 Ma period: less than 300 m Ma− 1/2 between 101° E and 120° E and less …