Basaltic magmas and mafic minerals Flashcards

1
Q

What does distribution of earths subaerial volcanoes give an insight into?

A

tectonic settings of magma generation

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2
Q

How are subaerial volcanoes usually found?

A

in long linear chains linked most commonly to convergent plate margins and subduction

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3
Q

What area is most important for magma generation?

A

Mid-ocean ridges

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4
Q

What are isolated sub-aerial volcanoes linked to?

A

Hotspots and mantle plumes (very hot magma melt surface) lead to creation of island arcs (Hawaii)

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5
Q

What is volcanism a manifestation of?

A

magma reaching the surface

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6
Q

Where will you find volcanic arcs?

A

destructive convergent plate margins

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7
Q

Where will you find rift valleys/ mid ocean ridges?

A

Divergent/ constructive plate boundaries

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8
Q

What are mantle plumes associated with?

A

intraplate volcanism (hotspots)

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9
Q

What leads to the generation of primary magmas?

A

partial melting

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10
Q

What does mantle melting lead to the production of in the crust?

A

igneous rocks

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11
Q

What is the mantle rock?

A

Lherzolite – the type of peridotite within
the upper mantle

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12
Q

What will peridotite be like?

A

mixture of minerals
Assemblage:
olivine, orthopyroxene, clinopyroxene
garnet (spinel low pressure, even low pressure plagioclase)

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13
Q

What can a rock be defined by?

A

bulk chemistry

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14
Q

How is bulk chemistry often defined?

A

in terms of wt% of oxides of major elements

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15
Q

Why does the mantle undergo partial melting? (general not examples)

A

this will be due how the geotherm and solidus interact

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16
Q

What is the solidus and how does it relate partial melting?

A

the solidus is the line which define if melting will occur if crossed due to higher temp or pressure

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17
Q

What will cause partial melting at mid-ocean ridges?

A

decompression melting

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18
Q

What is decompression melting?

A

hot mantle upwelling in response to divergence which reduces pressure

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19
Q

What will cause partial melting of mantle at mantle plumes?

A

hot mantles ascending to lower pressures

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20
Q

What is flux melting and how does lead to partial melting at subduction zones?

A

water added lowering the melting point

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21
Q

Will the mantle undergo full melting?

A

no only a small proportion (20-30%)

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22
Q

What does the proportion of rock melt depend on?

A

extent to which conditions exceed the solidus

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23
Q

How does partial melting affect chemical composition?

A

melt formed will not be same composition as mantle lherzolite

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24
Q

What does partially mantle peridotite produce?

A

broadly basaltic composition

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25
What do we call melts sourced directly from the mantle?
primary magmas
26
What is the density of mantle peridotite?
3300kg/m*3
27
What is the density of basaltic magma?
2700kg/m*3
28
What does the difference between densities of mantle peridotite and basaltic magma give basaltic liquids?
buoyancy- ascend upward to pressure gradient
29
What will buoyancy do to primary magmas?
drive it to crustal levels where they lose heat and start to crystallise
30
What can basalts that lie at the low-silica range of volcanic rocks also be referred to as?
basic magmas or mafic magmas due to common occurrence Fe- and Mg or Primitive magmas (close to primary composition)
31
What is the counterpart to primitive magmas?
evolved - rich silica and alkali rich
32
What are evolved magmas also referred to as?
acidic magmas or felsic (common occurrence in feldspar and quartz)
33
What happens after magmas ascend from the mantle?
they may stall and completely solidify forming intrusive igneous rocks or erupt on surface forming extrusive igneous rocks
34
What happens if basaltic magma cool and completely crystallise without further modifiction?
will form rocks of the same composition
35
What will the cooling rate of basaltic magma control?
coarsely or finely crystalline
36
What will fine grain rock formed from cooling basaltic lava be called?
basalt
37
What will coarse grain rock formed from cooling basaltic lava be called?
gabbro
38
What are the common minerals in basalt and gabbro?
Olivine Pyroxene Plagioclase feldspar
39
What is the structure of olivine?
isolated silicate tetrahedra with 2 cations per tetrahedra balancing charge
40
What are the 2 end members for the solid solution of olivine?
Forsterite - Mg Fayalite- Fe
41
What important general principle for the chemical evolution of magmas can be highlighted by depletion of minerals in liquid?
composition of crystals growing in liquid aren't the same as composition of liquid thus liquid composition evolves through crystallisation
42
What is the colour property olivine?
Olive green / greenish-yellow in hand
43
What will crystals be like in olivine?
granular masses of blocky to rounded crystals
44
What will cleavage be like in olivine?
no good cleavage (but often has curved fractures in thin section)
45
What is olivine prone to at lower temp?
alteration- often visible in thin sections
46
What are the optical properties of olivine in thin section?
Colourless - ppl High relief Equant blocky grain (6 sided) rounded/ sub-rounded No cleavage but curved cracks Mid-high second order birefringence
47
What is the structure of pyroxenes?
single-chain silicate tetrahedra (joined by shared Si) cation in between balancing charge
48
What 2 distinct series can pyroxenes be split into based upon crystal structure?
Orthopyroxene (orthorhombic) Clinopyroxene (monoclinic)
49
What are the properties of pyroxene crystals?
Dark green to black colour in hand specimen Short stubby prisms square to eight side in cross section
50
What are the optical properties of pyroxenes in thin section for ppl?
Colourless to pale pink (opx), colourless to pale brown/green (cpx) Moderate relief Often 1 good cleavage visible 2 in end section
51
What are the optical properties of pyroxenes in thin section xpl for orthopyroxene?
First order birefringence (yellow grey) Straight extinction relative to cleavage
52
What are the optical properties of pyroxenes in thin section xpl for Clinopyroxene?
Up to second order birefringence Inclined extinction relative to cleavage
53
What is plagioclase feldspar like in hand specimen?
white blocky crystals
54
What is plagioclase feldspar like in hand specimen?
low relief colourless low first order birefringence
55
What is plagioclase feldspar like in xpl?
Very distinctive lamellar twinning (black/grey/white stripes)
56
What can the assemblage of a rock be thought of as?
related "family" of minerals which reflect bulk chemistry of magma crystallised from
57
How many minerals will igneous rocks by predominantly comprised of?
3 or 4
58
What is the amphibole mineral group like?
common in intermediate igneous as well as evolved
59
What is an example of an amphibole?
Hornblende
60
What is the structure of hornblende like?
Double chain silicate large ionic site
61
What does the large ionic site of of hornblende mean it can accomodate?
hydroxyl (OH) ions
62
What will hornblende be like in hand specimen?
crystals prismatic and dark coloured (black/ dark brown) Lozenge shape end section
63
What is hornblende like in thin section ppl?
brown or green colour strong pleochroism moderate relief
64
What is hornblende like in thin section xpl?
Up to low second-order birefringence Well-developed cleavage
65