| 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. |
| Genre: | Article |
| ProdID: | 70010484 |
| Citation Author: | Barnes, I.; Lamarche, Jr. , V. C.; Himmelberg, G. |
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| Citation End Page: | 832 |
| Citation Issue: | 3776 |
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| Citation Language: | English |
| Citation Larger Work Title: | Science |
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| Citation Number Of Pages: | 3 |
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| Citation Search Results Text: | Geochemical evidence of present-day serpentinization; 1967; Article; Journal; Science; Barnes, I.; Lamarche, Jr. , V. C.; Himmelberg, G. |
| Citation Start Page: | 830 |
| Citation Volume: | 156 |
| Citation Year: | 1967 |
| Type: | citation/reference |
| Text: | Geochemical evidence of present-day serpentinization; 1967; Article; Journal; Science; Barnes, I.; Lamarche, Jr. , V. C.; Himmelberg, G. |
| URL (THUMBNAIL): | http://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg |
| Date Other: | Sun, 1 Jan 1967 00:00 -0600 |
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