Nature geoscience - volume 4 issue 1, january 2011
Nature geoscience - volume 4 issue 1, january 2011"
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Continental rifting creates narrow ocean basins, where coastal ocean upwelling and enhanced silicate weathering remove carbon dioxide from the atmosphere. Evidence from seismic data, sonar
backscatter and seafloor images, and geochemical water analyses suggest that in young sedimented rifts, active magmatism occurs in a broader region than appreciated and releases carbon from
the sediments.
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