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Granitic intrusions enhance strain localization and rapid mantle exhumation along an oceanic detachment fault
Abstract INTRODUCTION RESULTS DISCUSSION MATERIALS AND METHODS Acknowledgments Supplementary Materials REFERENCES Information & Authors Metrics & Citations View Options References Figures Tables Media Share Abstract Serpentinization and magmatism weaken the lithosphere and facilitate mantle exhumation during magma-poor rifting and ultraslow seafloor spreading. However, the complex interplay and timing among these competing mechanisms along detachment faults remain poorly constrained.
Li isotope ratios of spring fluids as an effective tracer of slab-derived subducted sources across the Costa Rica forearc
Spring waters from across the Costa Rica margin were analyzed for their Li and He isotope compositions to determine the utility of Li isotopes as a tracer of volatile sources in subduction zones. Li isotope ratios systematically decrease with increasing depth to the subducting slab: averaging +15.0‰ ± 9.2‰ in the outer forearc (80 km to the slab).
Chlorine Isotope Fractionation of the Major Chloromethane Degradation Processes in the Environment
Download Hi-Res ImageDownload to MS-PowerPointCite This:Environ. Sci. Technol. 2019, XXXX, XXX RETURN TO ARTICLES ASAPPREVArticleNEXT Frank Keppler* Jaime D. Barnes Jaime D.
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