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Heterogeneous cooling subsidence of spreading oceans controlled by spreading rate
Ocean spreading is an intergral part of the Wilson cycle and its dynamics crucially reflects global tectonic processes. Ocean age-dependent cooling subsidence with seafloor deepening is traditionally described by models of thermochemical buoyancy of oceanic plates with globally constant parameters, that specify a linear correlation between square-root ...openaire +1 more source
2000
Primary melts generated in the oceanic mantle migrate upward and pond at major discontinuities to form magma chambers. Such chambers have thus far been identified only on fast- and intermediate-spreading ridges but probably also exist at slow-spreading ridges.
Malpas, J, Robinson, PT
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Primary melts generated in the oceanic mantle migrate upward and pond at major discontinuities to form magma chambers. Such chambers have thus far been identified only on fast- and intermediate-spreading ridges but probably also exist at slow-spreading ridges.
Malpas, J, Robinson, PT
openaire +2 more sources
Calcium isotopic compositions of oceanic crust at various spreading rates
Geochimica Et Cosmochimica Acta, 2020Chunfei Chen +2 more
exaly
The oceanic crustal structure at the extinct, slow to ultraslow Labrador Sea spreading center
Journal of Geophysical Research: Solid Earth, 2015Matthias Delescluse +2 more
exaly