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.
What “melting” produces a lot of magma?
Decompression Melting
Where can magma form?
- Mid-oceanic ridges
- Mantle plumes (hot spots)
- Subduction Zones
Why and how magma rises?
Since magma is less dense than the surrounding country rock, it rises faster when the difference in density between the magma and the surrounding rock is greater.
MAGMA FACTORS to VISCOSITY
- Higher Temperature means?
- Higher Silica Content means?
- Higher content of H2O means?
- Lower Viscosity
- Higher Viscosity
- Lower Viscosity
Explain Bowen’s Reaction Series
Minerals that Crystallizes First (In Order): • Olivine • Plagioclase Feldspar • Amphibole and Biotite • Muscovite Mica and Potassium Feldspar • Quartz