Boron isotope systematics of slab fluids as inferred from a serpentine seamount, Mariana forearc
Authors:
- Laurie D. BentonLBLaurie D. Benton
- Jeffrey G. RyanJRJeffrey G. Ryan
- Fouad TeraFTFouad Tera
- 1 May 2001
- journal article
- Published by Elsevier in Earth and Planetary Science Letters
- Vol. 187 (3-4) , 273-282
Abstract
No abstract availableKeywords
This publication has 39 references indexed in Scilit:
- Two isotopically distinct fluid components involved in the Mariana arc: Evidence from Nb/B ratios and B, Sr, Nd, and Pb isotope systematicsGeology, 1999
- The boron systematics of intraplate lavas: Implications for crust and mantle evolutionGeochimica et Cosmochimica Acta, 1996
- Cross-Arc Geochemical Variations in the Kurile Arc as a Function of Slab DepthScience, 1995
- Primitive Boron Isotope Composition of the MantleScience, 1995
- Boron isotope systematics of marine sedimentsEarth and Planetary Science Letters, 1993
- Separating mantle from slab signatures in arc lavas using B/Be and radiogenic isotope systematicsNature, 1993
- Mobilization of boron in convergent margins: Implications for the boron geochemical cycleGeology, 1993
- Origin of waters responsible for serpentinization of the Izu-Ogasawara-Mariana forearc seamounts in view of hydrogen and oxygen isotope ratiosEarth and Planetary Science Letters, 1990
- An improved method for the high-precision isotopic measurement of boron by thermal ionization mass spectrometryInternational Journal of Mass Spectrometry and Ion Processes, 1988
- Serpentinization of oceanic peridotites: temperature dependence of mineralogy and boron contentEarth and Planetary Science Letters, 1984