Melts and fluids evolution in the process of crust and mantle formation in Paleo-Proterozoic (2,2—1,75 Ga ago). Stratigraphy and magnetic activity
Stratigraphy of metamorphic Precambrian complexes related to Paleo-Proterozoic is controversial. An additional sign permitting to correlate strata may be their material composition because in the Precambrian composition of deep fluids changed regularly. Then some regularity in changes of compositio...
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| Formaat: | Artigo |
| Taal: | Inglês |
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Subbotin Institute of Geophysics of the National Academy of Sciences of Ukraine
2017-06-01
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| Reeks: | Геофизический журнал |
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| Online toegang: | https://journals.uran.ua/geofizicheskiy/article/view/97383 |
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