Boron isotope geochemistry of the oceanic crust from DSDP/ODP Hole 504B
- 14 April 1992
- journal article
- Published by Elsevier in Geochimica et Cosmochimica Acta
- Vol. 56 (4) , 1633-1639
- https://doi.org/10.1016/0016-7037(92)90230-g
Abstract
No abstract availableKeywords
This publication has 29 references indexed in Scilit:
- Serpentinization of oceanic peridotites: temperature dependence of mineralogy and boron contentPublished by Elsevier ,2002
- Tourmaline mineralization in the Barberton greenstone belt, South Africa: early Archean metasomatism by evaporite-derived boronContributions to Mineralogy and Petrology, 1991
- Suppression of boron volatilization from a hydrofluoric acid solution using a boron-mannitol complexAnalytical Chemistry, 1990
- Distribution et comportement du bore dans la croûte océaniqueCanadian Journal of Earth Sciences, 1989
- Distribution of alteration zones in the upper oceanic crustGeology, 1988
- Strontium, oxygen, and hydrogen isotope geochemistry of hydrothermally altered and weathered rocks in DSDP Hole 504B, Costa Rica RiftEarth and Planetary Science Letters, 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
- In situ electrical resistivity and bulk porosity of the oceanic crust Costa Rica RiftNature, 1982
- DSDP Hole 504B, the first reference section over 1 km through Layer 2 of the oceanic crustNature, 1982
- Strontium and oxygen isotopic composition of some basalts from Hole 504B, Costa Rica Rift, DSDP Legs 69 and 70Earth and Planetary Science Letters, 1982