Abstract
Research was carried out into Early Proterozoic metamorphic formations in the mobile Shackleton ridge. This made it possible to trace the cyclicity in the development of the metamorphic complex. A cryometric method of correlating CH4/CO2 in inclusions in the lgfO2 field was used to ascertain the distribution of carbon dioxide-methane fluid, and the results agreed with results obtained by mass-spectrometry and gas chromatography. -P.Cooke
| Original language | English |
|---|---|
| Pages (from-to) | 65-76 |
| Number of pages | 12 |
| Journal | Izvestiya - Akademiya Nauk SSSR, Seriya Geologicheskaya |
| Volume | 3 |
| State | Published - 1 Jan 1991 |
| Externally published | Yes |
ASJC Scopus subject areas
- General Environmental Science
- General Earth and Planetary Sciences
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