Volcanism at constructive plate margins Flashcards

1
Q

Name a type constructive plate margin setting.

A

Mid-ocean ridges.

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2
Q

What type of melting occurs at constructive plate margins?

A

Adiabatic decompression melting.

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3
Q

What is adiabatic decompression melting?

A

Where no heat is transferred between the system and the surroundings.

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4
Q

Describe the positions of the geothermal and solidus at constructive plate margins.

A

The geothermal crosses the solidus at a shallow depth.

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5
Q

Explain how the geothermal crosses the solidus at a shallow depth.

A

Pressure on the mantle is reduced by lithospheric thinning.

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6
Q

What is the eruption temperature at constructive plate margins?

A

1,100C.

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7
Q

What type of magma is erupted at constructive plate margins?

A

Basaltic.

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8
Q

What type of basalt is mid-ocean ridge basalt (MORB)?

A

Tholeiitic.

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9
Q

Describe tholeiitic basalt.

A

Al and Mg-rich and K-poor.

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10
Q

How are tholeiitic basalts formed?

A

Higher degrees of partial melting.

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11
Q

Give two examples of common types of tholeiitic basalts/

A

Olivine and quartz tholeiites.

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12
Q

What type of mantle rock is melted to produce basaltic magma?

A

Ultramafic mantle rocks.

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13
Q

Why can’t MORB be a primary melt?

A

It is not in equilibrium with mantle olivine.

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14
Q

Describe fast spreading ridges.

A

They have smooth topography, a homogenous crust, and a robust magma supply.

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15
Q

Describe slow spreading ridges.

A

They have rugged topography with normal faulting, a heterogenous crust, and a variable magma supply.

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16
Q

How does trace element content in MORB compare to OIB?

A

MORB is depleted in all trace elements compared to OIB.

17
Q

What can MORB do at low pressure?

A

Crystallise.

18
Q

What type of trace elements is MORB most depleted in?

A

Incompatible trace elements.

19
Q

Describe an incompatible trace element.

A

An element that is unsuitable in size/charge for the cation sites in its host mineral. It is not easily substituted into major element sites.