Comment on "Glacial cycles drive variations in the production of oceanic crust".

نویسنده

  • John A Goff
چکیده

Crowley et al. (Reports, 13 March 2015, p. 1237) propose that abyssal hill topography can be generated by variations in volcanism at mid-ocean ridges modulated by Milankovitch cycle-driven changes in sea level. Published values for abyssal hill characteristic widths versus spreading rate do not generally support this hypothesis. I argue that abyssal hills are primarily fault-generated rather than volcanically generated features.

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عنوان ژورنال:
  • Science

دوره 349 6252  شماره 

صفحات  -

تاریخ انتشار 2015