Geochemical evidence of present-day serpentinization
Science
By: I. Barnes, Valmore C. LaMarche Jr., and G. Himmelberg
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Abstract
Ultrabasic (pH > 11) water issues from some fresh ultramafic bodies. The properties of the ultrabasic solutions are believed to be due to current reactions yielding serpentine from primary olivines and pyroxenes. The low concentrations of divalent iron, divalent magnesium, and dissolved silica from the serpentinization require an increase in rock volume.
| Publication type | Article |
|---|---|
| Publication Subtype | Journal Article |
| Title | Geochemical evidence of present-day serpentinization |
| Series title | Science |
| Volume | 156 |
| Issue | 3776 |
| Year Published | 1967 |
| Language | English |
| Larger Work Type | Article |
| Larger Work Subtype | Journal Article |
| Larger Work Title | Science |
| First page | 830 |
| Last page | 832 |
| Google Analytic Metrics | Metrics page |