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Deep crustal carbonates as CO2 fluid sources: evidence from metasomatic reaction zones
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Published in: | Contributions to mineralogy and petrology 1983-03, Vol.84 (1), p.15-24 |
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Language: | English |
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cites | cdi_FETCH-LOGICAL-c258t-b94612d750ab59c6f7ebbbc1179799f6edff2463028470ea0d86376bcd4cd3c83 |
container_end_page | 24 |
container_issue | 1 |
container_start_page | 15 |
container_title | Contributions to mineralogy and petrology |
container_volume | 84 |
creator | GLASSLEY, W. E |
description | |
doi_str_mv | 10.1007/BF01132326 |
format | article |
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identifier | ISSN: 0010-7999 |
ispartof | Contributions to mineralogy and petrology, 1983-03, Vol.84 (1), p.15-24 |
issn | 0010-7999 1432-0967 |
language | eng |
recordid | cdi_crossref_primary_10_1007_BF01132326 |
source | SpringerLink Online Journals Archive Complete |
subjects | Crystalline rocks Earth sciences Earth, ocean, space Exact sciences and technology Igneous and metamorphic rocks petrology, volcanic processes, magmas |
title | Deep crustal carbonates as CO2 fluid sources: evidence from metasomatic reaction zones |
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