The shallow attenuation structure of the fast‐spreading East Pacific Rise near 9°30′N
- 1 March 1994
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 21 (5) , 321-324
- https://doi.org/10.1029/94gl00189
Abstract
No abstract availableKeywords
This publication has 19 references indexed in Scilit:
- The renavigation of Sea Beam bathymetric data between 9° N and 10° N on the East Pacific RiseMarine Geophysical Research, 1993
- The Seismic Attenuation Structure of a Fast-Spreading Mid-Ocean RidgeScience, 1992
- Structure of young upper crust at the East Pacific Rise near 9°30'NGeophysical Research Letters, 1992
- Q structure of the oceanic crustMarine Geophysical Research, 1991
- Hydrothermal vent distribution along the East Pacific Rise crest (9°09′–54′N) and its relationship to magmatic and tectonic processes on fast-spreading mid-ocean ridgesEarth and Planetary Science Letters, 1991
- The three-dimensional seismic velocity structure of the East Pacific Rise near latitude 9° 30′ NNature, 1990
- Flow porosities, permeabilities and preliminary data on fluid inclusions and fossil thermal gradients in the crustal sequence of the Sumail ophiolite (Oman)Tectonophysics, 1988
- Physical Mechanisms Contributing to Seismic Attenuation in the CrustPublished by Springer Nature ,1987
- Tectonics of the East Pacific Rise near 12°50′N: a submersible studyEarth and Planetary Science Letters, 1984
- Lava flow layer‐East Pacific RiseGeophysical Research Letters, 1982