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Crustal fluid–rock interactions, mass transfer and cycling of volatiles
| Content Provider | Scilit |
|---|---|
| Author | Wanty, Richard B. Ii, Robert R. Seal |
| Copyright Year | 2004 |
| Description | In general, the C of metamorphic rocks can have diverse sources. C can be derived from the mantle or lower levels of the Earth's crust with metamorphic fluid during the process of metamorphism. Alternatively, C may be inherited from the protoliths before their metamorphism. We can suggest that in cases where there is a sufficiently large resource of external C-bearing fluid, or if there is a high fluid/ rock ratio during metamorphism, the C isotopic composition of various rocks will be similar, on the average, regardless of the origin of the rock. However, in the case of metamorphic rocks with distinctly different C isotopic compositions, which can be certainly related to their lithologic composition, where there are limited external C-bearing fluids or the fluid/rock ratio was small, then the primary heterogeneity of the C isotopic composition of the protoliths would be little changed. We have examined the question of C sources and amounts of C-bearing fluid associated with metamorphism using of two metamorphic complexes in the eastern Siberia. Book Name: Water-Rock Interaction, Two Volume Set |
| Related Links | https://content.taylorfrancis.com/books/download?dac=C2014-0-34624-8&isbn=9780429080487&doi=10.1201/9781482284515-9&format=pdf |
| Ending Page | 350 |
| Page Count | 84 |
| Starting Page | 267 |
| DOI | 10.1201/9781482284515-9 |
| Language | English |
| Publisher | Informa UK Limited |
| Publisher Date | 2004-09-02 |
| Access Restriction | Open |
| Subject Keyword | Book Name: Water-Rock Interaction, Two Volume Set Isotopic Composition |
| Content Type | Text |
| Resource Type | Chapter |
