Magma Formation Flashcards
Process in magma differentiation where it combines and mixes magma.
Magma Mixing
Partial Melting
- It refers to a process that creates a magmatic melt from a portion of a solid rock less than the whole.
- refer to the geothermal graph
A chemical process by which the composition of a liquid, such as magma, changes due to crystallization.
Crystal Fractionation
Denser minerals crystallize first and settle down while the lighter minerals crystallize at the latter stages.
Crystal Settling
It is a complex process whereby a single melt can produce a wide variety of different igneous rocks.
Magmatic Differentiation
It results from the transfer of heat and decompression.
Magma Generation
The heat generated by long-term radioactive decay.
Radioactive Heat
The heat generated during the Earth’s formation.
Primordial Heat
A discontinuity between lower mantle and outer core.
Guttenberg Discontinuity
Explain Geothermal Gradient
- The temperature increase with depth into Earth.
- Pressure also plays a part when melting rocks. • Higher pressure means higher melting point.
- Thus, the gradient is not a straight line, but a curved one.
What is Magma?
Magma is defined as molten rock found below the earth’s surface. It’s a Greek word meaning ‘thick ointment.’
What are the composition of magma?
It is composed of whatever elements made up the minerals in the source rocks, since it is a variety of rocks that are melted therefore the composition is unclear.
Explain Decompression Melting
- Going back to the Geothermal Gradient graph, the rocks goes up decreasing its depth and pressure, but not the temperature.
- This allows the rock to melt at that temperature because of the lowered pressure.
- This usually happens in divergent boundaries. This creates new magma!
Explain Flux Melting
- Convergent Boundaries
- When the H2O from the descending plate (the denser plate) are compressed into the hotter mantle rocks above.
- Helps break the chemical bonds decreasing the melting point of the rock.
- This completely disorganizes the geothermal graph, pushing the partial melting and the liquid melting stage to the left, thus allowing melting.
Explain Heat Transfer Melting
• Due to the Flux Melting, some magma are stuck beneath the continental lithosphere above, the stuck magma melts the surrounding rocks.