Boron desorption and fractionation in Subduction Zone Fore Arcs: Implications for the sources and transport of deep fluids

Author:

Saffer Demian M.1ORCID,Kopf Achim J.2

Affiliation:

1. Department of Geosciences & Center for Geomechanics; Geofluids, & Geohazards, The Pennsylvania State University; University Park Pennsylvania USA

2. MARUM, Center for Marine Environmental Sciences, University of Bremen; Bremen Germany

Publisher

American Geophysical Union (AGU)

Subject

Geochemistry and Petrology,Geophysics

Reference89 articles.

1. On the geodynamics of the Aegean rift;Agostini;Tectonophysics,2010

2. Density, porosity, and compaction of sedimentary rocks;Athy;Am. Assoc. Pet. Geol. Bull.,1930

3. Seismic velocities from the Barbados Ridge complex: Indicators of high pore fluid pressures in an accretionary complex;Bangs;J. Geophys. Res.,1990

4. Boron isotope variations in nature: A synthesis;Barth;Geol. Rundsch.,1993

5. Geometry and mechanisms of fluid flow at 15 to 45 kilometer depths in an early Cretaceous accretionary complex;Bebout;Geophys. Res. Lett.,1991

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