Variability in oceanic crustal thickness and structure: Multichannel seismic reflection results from the northern East Pacific Rise
- 10 August 1996
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 101 (B8) , 17951-17975
- https://doi.org/10.1029/96jb00814
Abstract
No abstract availableKeywords
This publication has 123 references indexed in Scilit:
- Ophiolites, seismic velocities and oceanic crustal structurePublished by Elsevier ,2003
- The East Pacific Rise and its flanks 8?18 N: History of segmentation, propagation and spreading direction based on SeaMARC II and Sea Beam studiesMarine Geophysical Research, 1992
- Flow porosities, permeabilities and preliminary data on fluid inclusions and fossil thermal gradients in the crustal sequence of the Sumail ophiolite (Oman)Tectonophysics, 1988
- Mantle—crust transition zone and origin of wehrlitic magmas: Evidence from the Oman ophioliteTectonophysics, 1988
- Structural evolution of the East Pacific Rise axis from 13°10′N to 10°35′N: interpretations from SeaMARC I dataTectonophysics, 1987
- A rolling mill effect in asthenosphere beneath oceanic spreading centersEarth and Planetary Science Letters, 1984
- Mantle flow at oceanic spreading centers: Models derived from ophiolitesTectonophysics, 1982
- On long‐term thickening of the oceanic crustGeophysical Research Letters, 1981
- The structures of two ophiolite massifs, Bay-of-Islands, Newfoundland: A model for the oceanic crust and upper mantleTectonophysics, 1981
- Fine structure of the lower oceanic crust on the Cocos PlateTectonophysics, 1979