Geochemistry of hydrothermally altered oceanic crust: DSDP/ODP Hole 504B – Implications for seawater‐crust exchange budgets and Sr‐ and Pb‐isotopic evolution of the mantle
- 7 March 2003
- journal article
- Published by American Geophysical Union (AGU) in Geochemistry, Geophysics, Geosystems
- Vol. 4 (3)
- https://doi.org/10.1029/2002gc000419
Abstract
No abstract availableKeywords
This publication has 71 references indexed in Scilit:
- The geochemical consequences of late-stage low-grade alteration of lower ocean crust at the SW Indian Ridge: results from ODP Hole 735B (Leg 176)Geochimica et Cosmochimica Acta, 2001
- The uptake of carbon during alteration of ocean crustGeochimica et Cosmochimica Acta, 1999
- Rare earth element mobility in the oceanic lower sheeted dyke complex: evidence from geochemical data and leaching experimentsChemical Geology, 1998
- Unusually large NbTa depletions in North Chile ridge basalts at 36°50′ to 38°56′S: major element, trace element, and isotopic dataEarth and Planetary Science Letters, 1996
- Sulfur isotopic profile through the oceanic crust: Sulfur mobility and seawater-crustal sulfur exchange during hydrothermal alterationGeology, 1995
- Microstructural evolution of a deformation zone in the upper ocean crust: Evidence from DSDP hole 504BJournal of Geodynamics, 1991
- The geochemistry of sulfur in a 1.3 km section of hydrothermally altered oceanic crust, DSDP Hole 504BGeochimica et Cosmochimica Acta, 1989
- 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
- Strontium and oxygen isotopic composition of some basalts from Hole 504B, Costa Rica Rift, DSDP Legs 69 and 70Earth and Planetary Science Letters, 1982
- On the effect of low-temperature seawater-basalt interaction on the distribution of sulfur in oceanic crust, layer 2Earth and Planetary Science Letters, 1979