Comment on "Sensitivity of seafloor bathymetry to climate-driven fluctuations in mid-ocean ridge magma supply"

被引：13

作者：

Huybers, Peter ^{[1
]}

Langmuir, Charles ^{[1
]}

Katz, Richard F. ^{[3
]}

Ferguson, David ^{[1
]}

Proistosescu, Cristian ^{[1
]}

Carbotte, Suzanne ^{[2
]}

机构：

[1] Harvard Univ, Cambridge, MA 02138 USA

[2] Lamont Doherty Earth Observ, Palisades, NY USA

[3] Univ Oxford, Oxford, England

来源：

SCIENCE | 2016年 / 352卷 / 6292期

基金：

美国国家科学基金会;

关键词：

GALAPAGOS-SPREADING-CENTER; MID-ATLANTIC-RIDGE; DE-FUCA RIDGE; CRUSTAL THICKNESS; OCEANIC-CRUST; MORPHOLOGY;

D O I：

10.1126/science.aae0451

中图分类号：

O [数理科学和化学]; P [天文学、地球科学]; Q [生物科学]; N [自然科学总论];

学科分类号：

07 ; 0710 ; 09 ;

摘要：

Olive et al. (Reports, 16 October 2015, p. 310) argue that similar to 10% fluctuations in melt supply do not produce appreciable changes in ocean ridge bathymetry on time scales less than 100,000 years and thus cannot reflect sea level forcing. Spectral analysis of bathymetry in a region they highlight as being fault controlled, however, shows strong evidence for a signal from sea level variation.

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页数：2

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