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From slow to ultra-slow: How does spreading rate affect seafloor roughness and crustal thickness?

Daniel Sauter 1 Heather Sloan 2 Mathilde Cannat 3 John A. Goff 4 Philippe Patriat 3 Marc Schaming 1 Walter Roest 5 
1 IPGS-Dylbas - Dynamique de la lithosphère et des bassins sédimentaires (IPGS)
IPGS - Institut de physique du globe de Strasbourg
2 EGGS - Department of Environmental, Geographic and Geological Sciences [Lehman]
3 IPGP - Institut de Physique du Globe de Paris
4 Institute for Geophysics, Jackson School of Geosciences
5 GM - Géosciences Marines
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https://hal.archives-ouvertes.fr/hal-00721860
Contributor : Daniel Sauter Connect in order to contact the contributor
Submitted on : Monday, July 30, 2012 - 4:46:42 PM
Last modification on : Friday, March 18, 2022 - 11:40:02 AM

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Daniel Sauter, Heather Sloan, Mathilde Cannat, John A. Goff, Philippe Patriat, et al.. From slow to ultra-slow: How does spreading rate affect seafloor roughness and crustal thickness?. Geology, Geological Society of America, 2011, 39 (10), pp.907-910. ⟨10.1130/G32028.1⟩. ⟨hal-00721860⟩

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