Abstract
The Changbaishan Tianchi volcano is composed of the basaltic rocks at the shield-forming stage, the trachyte and pantellerite at the cone-forming stage and modern eruption. Studies on their REE, incompatible elements and Sr, Nd, Pb isotopes suggest that rocks at different stages have a common magma genesis and close evolution relationship with differentiation crystallization playing the key role. The co-eruption of basaltic trachyandesite magma and pantellerite magma indicates that there exist both crustal magma chamber and mantle magma reservoir beneath the Tianchi volcano.
| Original language | English |
|---|---|
| Pages (from-to) | 382-389 |
| Number of pages | 8 |
| Journal | Science in China, Series D: Earth Sciences |
| Volume | 41 |
| Issue number | 4 |
| Publication status | Published - Aug 1998 |
Keywords
- Changbaishan Tianchi volcano
- Geochemistry
- Magma evolution
- Petrology
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