Microstructural evolution of a deformation zone in the upper ocean crust: Evidence from DSDP hole 504B
- 1 January 1991
- journal article
- Published by Elsevier in Journal of Geodynamics
- Vol. 13 (2-4) , 119-140
- https://doi.org/10.1016/0264-3707(91)90035-d
Abstract
No abstract availableKeywords
This publication has 13 references indexed in Scilit:
- State of lithospheric stress and borehole stability at Deep Sea Drilling Project Site 504B, eastern equatorial PacificJournal of Geophysical Research, 1990
- Direct observation of a section through slow-spreading oceanic crustNature, 1989
- Proceedings of the Ocean Drilling Program, 111 Initial ReportsPublished by International Ocean Discovery Program (IODP) ,1988
- Marine tectonics: Processes at mid‐ocean ridgesReviews of Geophysics, 1987
- Hydrothermal alteration of a 1 km section through the upper oceanic crust, Deep Sea Drilling Project Hole 504B: Mineralogy, chemistry and evolution of seawater‐basalt interactionsJournal of Geophysical Research, 1986
- A Geothermal and Geophysical Survey on the South Flank of the Costa Rica Rift: Sites 504 and 505Published by International Ocean Discovery Program (IODP) ,1985
- Crystalline rocks as possible paleoseismicity indicatorsGeology, 1985
- Formation of uppermost oceanic crustTectonics, 1982
- Morphology and tectonics of the inner rift valley at lat 36°50′N on the Mid-Atlantic RidgeGSA Bulletin, 1977
- An Analysis of Near-Bottom Magnetic Anomalies: Sea-Floor Spreading and the Magnetized LayerGeophysical Journal International, 1975