Geology Of the Mantle Flashcards

(48 cards)

1
Q

Ultramafic Xenoliths

A

chunks of solid mantle carried upward as inclusions in lava

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2
Q

Chemical reactions and quantum mechanics

A

Ultramafic Xenoliths

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3
Q

Ophiolite

A

a chunk of seafloor that has been pushed up on land, we can detrmine the composition of the mantle by averaging it’s layers

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4
Q

a chunk of seafloor that has been pushed up on land, we can detrmine the composition of the mantle by averaging it’s layers

A

Ophiolite

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5
Q

layers of an ophiolite (bottom to top)

A

Hartzburgite, dunite, gabbro, sheet dikes, pillow bassalts

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6
Q

Hartzburgite, dunite, gabbro, sheet dikes, pillow bassalts

A

layers of an ophiolite (bottom to top)

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7
Q

Lherzolite

A

the forbidden rock we know exists, but can’t see, that makes up the upper mantle. Composed of Olovine, Orthopyroxine, and clinopyroxine

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8
Q

the forbidden rock we know exists, but can’t see, that makes up the upper mantle. Composed of Olovine, Orthopyroxine, and clinopyroxine

A

Lherzolite

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9
Q

Aluminum in the mantle

A

can’t be incorporated int Lherzolite, so insted it forms either plagioclase, spinel, or garnet depending on the conditions

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10
Q

can’t be incorporated int Lherzolite, so insted it forms either plagioclase, spinel, or garnet depending on the conditions

A

Aluminum in the mantle

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11
Q

Olivine collor in hand

A

olive green to greenish grey

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12
Q

olive green to greenish grey

A

Olivine collor in hand

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13
Q

olivine cleavage

A

poor cleavage, in both hand sample and thin section, thin section shows fracturing

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14
Q

poor cleavage, in both hand sample and thin section, thin section shows fracturing

A

olivine cleavage

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15
Q

Olivine habbit

A

either massive or drusty

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16
Q

either massive or drusty

A

Olivine habbit

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17
Q

olivine XPL

A

second order collors like a stained glass window

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18
Q

second order collors like a stained glass window

A

olivine XPL

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19
Q

clinopyroxene in thin section

A

bright 2nd order olors in XPL, has obvious cleavage

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20
Q

bright 2nd order olors in XPL, has obvious cleavage

A

clinopyroxene in thin section

21
Q

Orthopyroxene in thin section

A

1st order colors n XPL with obvious cleavage

22
Q

1st order colors n XPL with obvious cleavage

A

Orthopyroxene in thin section

23
Q

pyroxenes in hand sample

A

nerely impossible to tell orthopyroxine and clinopyroxine appart, forms augite, tends to have hard to see 90 degree cleavage and never has twinning

24
Q

nerely impossible to tell orthopyroxine and clinopyroxine appart, forms augite, tends to have hard to see 90 degree cleavage and never has twinning

A

pyroxenes in hand sample

25
Plagioclase in thin section
first order collros with high probability of twinning
26
first order collros with high probability of twinning
Plagioclase in thin section
27
plagioclase in hand sample
grey to black, twinning is visible in larger crystals, such as in abrodorite, as streaks when held up to light.
28
grey to black, twinning is visible in larger crystals, such as in abrodorite, as streaks when held up to light.
plagioclase in hand sample
29
Garnet in thin section
constantly extinct in XPL, clear in PPL with high relief
30
constantly extinct in XPL, clear in PPL with high relief
Garnet in thin section
31
Garnet in hand
has hackley fracture and a distinctive crystal shape, usualy red, but not reliably so
32
has hackley fracture and a distinctive crystal shape, usualy red, but not reliably so
Garnet in hand
33
spinel hand sample
Magnetite, easily identified by magnetic properties and oxidized metalic luster, tends to grow in oxtahedral shapes
34
Magnetite, easily identified by magnetic properties and oxidized metalic luster, tends to grow in oxtahedral shapes
spinel hand sample
35
Pyroxene silicate structure
single chains bound together by octahedral groups of the smaller catioic membe (Usualy magnesium) Larger cations glue the layers together
36
single chains bound together by octahedral groups of the smaller catioic membe (Usualy magnesium) Larger cations glue the layers together
Pyroxene silicate structure
37
exsolution in thin section (lamelle)
fracture lines appear large/bold, because that is where the unwanted stuff is being shoved
38
fracture lines appear large/bold, because that is where the unwanted stuff is being shoved
exsolution in thin section (Lamelle)
39
orthopyroxene composition
(Mg,Fe) Si2O6, also known as pidgeonite when a little calcium is added in
40
(Mg,Fe) Si2O6, also known as pidgeonite when a little calcium is added in
orthopyroxene composition
41
clinopyroxine composition
(Mg,Ca) Si2O6, also known as augite, may include some iron
42
(Mg,Ca) Si2O6, also known as augite, may include some iron
clinopyroxine composition
43
Lhersolite
a dense mixture of clino/.orthopyrocine and olivine that forms under high pressure, the olivine alighns it's c axis along with the direction of mantle convection
44
a mix of clino/.orthopyrocine mixed with olivine
Lhersolite
45
Olivine structure
(Mg,Fe)SIO4 Has a TOT structure similar to pyroxene, alhtough it's an ortosylicate instead of a chain. calcium glues the structures together
46
(Mg,Fe)SIO4 Has a TOT structure similar to pyroxene.alhtough it's an ortosylicate instead of a chain. calcium glues the structures together
Structure of Olivine
47
Structure of Garnet
(Ca, Fe, Mg,)3Al2(SiO4)3. has a TOT arrangement
48
(Ca, Fe, Mg,)3Al2(SiO4)3. has a TOT arrangement
Structure of Garnet