Magma Formation Flashcards

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1
Q

Process in magma differentiation where it combines and mixes magma.

A

Magma Mixing

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2
Q

Partial Melting

A
  • 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
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3
Q

A chemical process by which the composition of a liquid, such as magma, changes due to crystallization.

A

Crystal Fractionation

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4
Q

Denser minerals crystallize first and settle down while the lighter minerals crystallize at the latter stages.

A

Crystal Settling

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5
Q

It is a complex process whereby a single melt can produce a wide variety of different igneous rocks.

A

Magmatic Differentiation

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6
Q

It results from the transfer of heat and decompression.

A

Magma Generation

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7
Q

The heat generated by long-term radioactive decay.

A

Radioactive Heat

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8
Q

The heat generated during the Earth’s formation.

A

Primordial Heat

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9
Q

A discontinuity between lower mantle and outer core.

A

Guttenberg Discontinuity

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10
Q

Explain Geothermal Gradient

A
  • 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.
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11
Q

What is Magma?

A

Magma is defined as molten rock found below the earth’s surface. It’s a Greek word meaning ‘thick ointment.’

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12
Q

What are the composition of magma?

A

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.

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13
Q

Explain Decompression Melting

A
  • 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!
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14
Q

Explain Flux Melting

A
  • 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.
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15
Q

Explain Heat Transfer Melting

A

• Due to the Flux Melting, some magma are stuck beneath the continental lithosphere above, the stuck magma melts the surrounding rocks.

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16
Q

What “melting” produces a lot of magma?

A

Decompression Melting

17
Q

Where can magma form?

A
  • Mid-oceanic ridges
  • Mantle plumes (hot spots)
  • Subduction Zones
18
Q

Why and how magma rises?

A

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.

19
Q

MAGMA FACTORS to VISCOSITY

  • Higher Temperature means?
  • Higher Silica Content means?
  • Higher content of H2O means?
A
  • Lower Viscosity
  • Higher Viscosity
  • Lower Viscosity
20
Q

Explain Bowen’s Reaction Series

A
Minerals that Crystallizes First (In Order):
• Olivine
• Plagioclase Feldspar
• Amphibole and Biotite
• Muscovite Mica and Potassium Feldspar
• Quartz