Comment on “Glacial cycles drive variations in the production of oceanic crust”-Reference-Cited by-同舟云学术

Comment on “Glacial cycles drive variations in the production of oceanic crust”

Published:2015-09-04 Issue:6252 Volume:349 Page:1065-1065
ISSN:0036-8075
Container-title:Science
language:en
Short-container-title:Science

Author:

Goff John A.¹

Affiliation:

1. Institute for Geophysics, Jackson School of Geosciences, University of Texas at Austin, Austin, TX, USA.

Abstract

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.

Publisher

American Association for the Advancement of Science (AAAS)

Subject

Multidisciplinary

Reference14 articles.

1. Glacial cycles drive variations in the production of oceanic crust

2. Mid‐ocean ridge eruptions as a climate valve

3. Stochastic analysis of seafloor morphology on the flank of the Southeast Indian Ridge: The influence of ridge morphology on the formation of abyssal hills

4. Abyssal hill characterization at the ultraslow spreading Southwest Indian Ridge

5. Incorporating “sinuous connectivity” into stochastic models of crustal heterogeneity: Examples from the Lewisian gneiss complex, Scotland, the Franciscan formation, California, and the Hafafit Gneiss Complex, Egypt

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