Magma And Intrusive Structures Flashcards

(62 cards)

1
Q

Melting of source rocks

A

Anatexis

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2
Q

requires that the melt remains in contact with the residual rock throughout the melting process. As a result, the overall composition of the system remains the same

A

Equilibrium melting

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3
Q

Implies that solids and melt separate into isolated fractions that do not continue to react together during the melting process.

A

Fractional melting

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4
Q

Earth ’ s average geothermal gradient is?

A

∼ 25 ° C/km for the upper 10km

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5
Q

geothermal gradient variation for old rocks

A

5-10C/km

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6
Q

Geo gradiemd for hotspots

A

30 to 50C/km

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7
Q

Decompression melting, also known as , results from a decrease in pressure.

A

adiabatic melting?

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8
Q

CO, CO2 , OH, SO2 , H2S, NH3 , K2O, Na2O, HCl and HF, as well as the elements H, F, Cl, S, He and Ar

A

Volatiles

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9
Q

A is an agent that reduces the melting temperature

A

flux

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10
Q

H2O, CO2 , K2O and Na2O is the major cause for partial melting in subduction zones. T or f

A

T

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11
Q

original melt evolves into one or more melts with a different composition, without material being exchanged with an external source

A

Differentiation

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12
Q

processes whereby early formed crystals are segregated from the remaining melt

A

Fractional crystallization

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13
Q

father of modern petrology

A

Bowen

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14
Q

Sill studied by bowen

A

Palisades sill

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15
Q

Coarse grained basalt

A

Diabase

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16
Q

indicate incomplete discontinuous chemical reactions between crystals and melts

A

Rxn rims

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17
Q

Bc they do not react with the magma, continuously or discontinuously

A

muscovite, potassium feldspar and quartz

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18
Q

Models for fractional crystallization

A

marginal accretion, gravitational separation, convective fl ow and filter pressing.

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19
Q

Crystallization along the walls of the magma chamber

A

marginal accretion

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20
Q

includes crystal settling and crystal flotation processes

A

Gravitational separation

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21
Q

one parent magma fractionates to produce two or more distinctly different daughter magmas with different compositions

A

Liquid fractionation

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22
Q

Liquid fractionation processes include (2)

A

differential diffusion and liquid immiscibility

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23
Q

involves the preferential diffusion of select ions within the magma in response to compositional, thermal or density gradients as well as water content. Differential diffusion may play a key role in the transport and concentration of metallic ore deposits in plutonic systems

A

Differential diffusion

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24
Q

, also called liquid – liquid fractionation , occurs when magma separates into two or more distinct immiscible liquid phases

A

Liquid immiscibility

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25
Forceful injection of magma commonly fractures the surrounding wall rock by a process called _ . Country rock fragments that fall ( stope ) into the magma are called_
stoping, xenoliths
26
involving multiple magma injections over time, produces complex relationships and constitutes an important diversification mechanism
Magma replenishment
27
occurs when two or more dissimilar magmas coexist, displaying contact relations but retaining their distinctive individual magma characteristics
Magma mingling
28
marble cake is caused by?
Magma mingling
29
implies thorough mixing so that the individual magma components are no longer recognizable. For example, felsic and mafi c magma can mix to produce an intermediate magma
Magma mixing
30
consists of genetically related magmas that have changed composition from a common original parental magma
magma series
31
Igneous rock series include: (2)
alkaline (or alkalic), and (2) sub - alkaline assemblages
32
high Na2O and K2O concentrations compared to SiO2 and are generally undersaturated with respect to SiO2
Alkaline
33
subalkaline series can be subdivided into (2)
calc alkaline and tholeiite suites
34
rocks have moderate to high Na2O, K2O and SiO2 concentrations
Calc alkaline
35
have low Na2O and K2O but high FeO and CaO concentrations
Tholeiites
36
Standard references include
Chondrite, primitive mantle, NMORB, EMORB, OIB
37
Useful in demonstrating enrichment or depletion of compatible VS incompatible elements
Spider diagram
38
Depletion of europium indicates plag fractionation from melt. T or f
T
39
Enrichment of europium indicates assimilation of plag. T or f
T
40
Calc alkali series include
Dacite, rhyolite, andesite, high alumina basalt(16-50%al2o3)
41
Magmas that dominate convergent e.g. Circum pacific
Calc alk
42
Rocks in convergent margin volcanoes are known as?
BADR
43
Al203 (Inc, Dec) with crystallization of ferromag monerals(olivine, Pyro, amphi) then (Inc, Dec) with removal of plag and micas
Inc, dec
44
MgO and Fe203 (Inc, Dec) with crystallization of ferromag min
Dec
45
Cao (Inc, Dec) with crystallization of Calc plag
Dec
46
NaO (Inc, Dec) due to removal of ig MgO Fe203 CaO, then (Inc, Dec) as sodium plag crystallizes in andesitic and more silicic rocks
Inc, dec
47
Sio2 and k20 (Inc, Dec) as MgO Fe203 CaO na203 Al203 are progressively removed by crystallization
Inc
48
_magmas and basalts dominate extensional envi e.g. Ocean ridges and cont drifts
Tholeiitic
49
Tholeiites occur over Hotspot in intra plate settings and in frontal portions of immature (relatively young) volc. Arcs (characterized by thinning crust). T or f
T
50
Amphi mins from alkaline magmas include
Riebeckite, richterite
51
Pryxn mins from alkaline rocks
Aegerine, aegirine-augite, spodumene
52
Alkaline rocks
Alkali basalts, hawaiite, benmoreite, mugearite, trachyte, nephelinite, phonolite, lamprophyre, carbonatite, komatiite, kimberlite
53
Alkali rocks occurs in?
Stable cratonic interior, cont rifts, ocean islands away from spreading centers and subd zones ,
54
Both alkali and tholeiitic magmas occur at hotspots, ocean islands, Rift envi. T or f
T
55
Calc alkaline occur almost at convergent margins. T or f
T
56
Tholeiitic magmas generated at ocean spreading centers, in cont rifts, Backarc basins, ocean islands, hotspots. T or f
T
57
Alkaline magmas occur primarily at hotspots, ocean islands, Rift. T or f
T
58
Bomodal rifts occur at cont rifts. T or f
T
59
Magmas of Rift valley
Alk and bomodal
60
Volc. Arc magma
Calc. Alkali
61
Ocean Island magma
Tholeiitic and alkali
62
Ocean ridge magma
Tholeiitic