Week 5 Flashcards
Decompression melting
Melting that occurs as rock ascends due to a drop in confining pressure
Addition of volatiles
Lowers melting temperature
Increased temperature
Causes melting
Bowen’s reaction series
A concept by Bowen that illustrates the relationships between magma and the minerals crystallizing from it during the formation of igneous rocks
Magmatic differentiation
The process of generating more than one rock type from a single magma
Crystal setting
A process that occurs during the crystallization of magma in which earlier formed minerals are denser than the liquid portion and settle to the bottom of the magma chamber
Dike
A tabular shaped intrusive igneous figure that cuts through the surrounding rock
Sill
Intrusive deposit. A tabular igneous body that was intruded parallel to the layering of preexisting rock
Pluton
Magma displaces rock, the solidified magma structures that result from this are intrusions (plutons)
Batholith
Extrusive, a large mass of igneous rock that formed when magma was emplaced at depth, crystallized, and subsequently exposed by erosion
Explain the process of decompression melting
As hot mantle rock goes up, it moves into zones of lower pressure. The drop in pressure initiates decompression melting.
What role does water and other volatiles play in the formation of magma
They act as salt does to melt ice. Water causes rock to melt at lower temperatures. This happens mainly at convergent plate boundaries( cool oceanic lithosphere sink, heat and pressure drive water from it and brings it to the wedge of the mantle, making it hotter and leads to melting
What 3 locations (in class) that magma will form
Midocean ridge
Subduction zones
Mantle plumes
Describe the process of crystal settling
Earlier formed minerals are denser than the liquid portion and sink to the bottom of the magma chamber(makes the result richer in sodium potassium and silica
Process of magmatic differentiation
When the remaining melt solidifies, if it migrates into surrounding rock it will form a rock with mineral composition
Process of assimilation
Rocks get into the magma and their composition does as well
Process of magma mixing
2 chemically different magma bodies are going up and the more buoyant may rise faster. They eventually join and mix and the two masses blend
3 ways magma will form
- Decrease in pressure (no increase in temp)-decompression
- adding water
- Heating is crustal rocks above melting temp
Viscosity
Fluids resistance to flow
Volatile
Gaseous components of magma dissolved in the melt. Ready to vaporize at surface pressures
Aa
Lava flow that has a jagged blocky surface
Pahoehoe
Lava flow with a smooth to ropy surface