| Article ID | Journal | Published Year | Pages | File Type |
|---|---|---|---|---|
| 4699277 | Chemical Geology | 2012 | 10 Pages |
Abstract
⺠Chlorine geochemistry is a rough indicator of metamorphic grade and mineralogy. ⺠High chlorine concentrations are found in samples with high amphibole contents. ⺠High δ37Cl values (⥠~ 0.5â°) are reported in samples with high amphibole content. ⺠Low δ37Cl values (< ~ 0â°) are found in samples dominated by clays. ⺠AOC is a major Cl host in the subducting oceanic lithosphere.
Related Topics
Physical Sciences and Engineering
Earth and Planetary Sciences
Geochemistry and Petrology
Authors
Jaime D. Barnes, Miguel Cisneros,