SUMMARY
The solidus and liquidus temperatures of granite are not fixed due to its mineral composition, but rather exist within a range influenced by pressure. Specifically, for 'M-type' granite, the solidus temperature occurs when the last quartz crystallizes, while the liquidus temperature is reached when the last plagioclase or mafic mineral melts. The role of pressure in these processes is acknowledged in Bowen's Reaction Series and is further discussed in the Tulane University article on igneous rocks.
PREREQUISITES
- Understanding of Bowen's Reaction Series
- Knowledge of granite mineral composition
- Familiarity with the concepts of solidus and liquidus temperatures
- Basic geology, particularly regarding magma formation
NEXT STEPS
- Research the specific solidus and liquidus temperatures for 'M-type' granite under varying pressure conditions
- Study the implications of pressure on melting points in igneous rocks
- Examine the mineral composition of different granite types and their melting behaviors
- Explore the Tulane University article on igneous rocks for detailed insights on magma and crystallization
USEFUL FOR
Geologists, petrologists, and students studying igneous rock formation, particularly those interested in the melting behavior of granite under varying pressure conditions.