Multi-scalar structure at DSDP/ODP Site 504, Costa Rica Rift, III: faulting and fluid circulation. Constraints from integration of FMS images, geophysical logs and core data
- 1 January 1998
- journal article
- Published by Geological Society of London in Geological Society, London, Special Publications
- Vol. 136 (1) , 311-326
- https://doi.org/10.1144/gsl.sp.1998.136.01.26
Abstract
No abstract availableKeywords
This publication has 34 references indexed in Scilit:
- Ridge-Flank Alteration of Upper Ocean Crust in the Eastern Pacific: Synthesis of Results for Volcanic Rocks of Holes 504B and 896APublished by International Ocean Discovery Program (IODP) ,1996
- A mechanism for decoupling within the oceanic lithosphere revealed in the Troodos ophioliteNature, 1995
- Proceedings of the Ocean Drilling Program, 148 Initial ReportsPublished by International Ocean Discovery Program (IODP) ,1992
- Proceedings of the Ocean Drilling Program, 137 Initial ReportsPublished by International Ocean Discovery Program (IODP) ,1992
- Microstructural evolution of a deformation zone in the upper ocean crust: Evidence from DSDP hole 504BJournal of Geodynamics, 1991
- Drilling deep into young oceanic crust, Hole 504B, Costa Rica RiftReviews of Geophysics, 1989
- Proceedings of the Ocean Drilling Program, 111 Initial ReportsPublished by International Ocean Discovery Program (IODP) ,1988
- 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
- Initial Reports of the Deep Sea Drilling Project, 69Published by International Ocean Discovery Program (IODP) ,1983
- DSDP Hole 504B, the first reference section over 1 km through Layer 2 of the oceanic crustNature, 1982