Accretion, structure and hydrology of intermediate spreading-rate oceanic crust from drillhole experiments and seafloor observations
- 1 June 1992
- journal article
- Published by Springer Science and Business Media LLC in Marine Geophysical Research
- Vol. 14 (2), 93-123
- https://doi.org/10.1007/bf01204282
Abstract
No abstract availableKeywords
This publication has 89 references indexed in Scilit:
- Drilling deep into young oceanic crust, Hole 504B, Costa Rica RiftReviews of Geophysics, 1989
- Eruption styles of basalt in oceanic spreading ridges and seamounts: Effect of magma temperature and viscosityJournal of Geophysical Research, 1988
- An oxygen isotopic profile through the upper kilometer of the oceanic crust, DSDP Hole 504BEarth and Planetary Science Letters, 1986
- Permeability versus depth in the upper oceanic crust: In situ measurements in DSDP hole 504B, eastern equatorial PacificJournal of Geophysical Research, 1985
- Permeability, underpressures, and convection in the oceanic crust near the Costa Rica Rift, eastern equatorial PacificJournal of Geophysical Research, 1982
- East Pacific rise at 21°N: The volcanic, tectonic, and hydrothermal processes of the central axisEarth and Planetary Science Letters, 1981
- The mechanisms of heat transfer through the floor of the Indian OceanJournal of Geophysical Research, 1977
- Detailed near-bottom geophysical study of the Gorda RiseJournal of Geophysical Research, 1973
- A Model for the Horst and Graben Structure of Midocean Ridge Crests based upon Spreading Velocity and Basalt Delivery to the Oceanic CrustGeophysical Journal International, 1973
- Block Faulting on the Gorda RiseScience, 1968