Model Answer
1- The following two component phase diagram represents the
diopside-anorthite eutectic crystallization
1- Label all phases
present on the diagram
2- Define the following:
(a) liquidus:
The line
separating the field of all liquid from that of liquid plus crystals
(b) Solidus:
The line
separating the field of all solid from that of liquid plus crystals
3- Label and define the eutectic point
The point on a
phase diagram, where the maximum number of allowable phases are in equilibrium.
When this point is reached, the temperature must remain constant until one of
the phases disappears.
4- Illustrate with labeled drawing type
of textures you might expect at the right side of the diagram?
Ophitic texture
5- Trace the
crystallization path of the point (a).
The Path abfh on the diagram
2- Explain the role of temperature, viscosity, and gas content of the
magma in producing each of the following features
(a) Lava flow:
If the liquid part of the magma has a low viscosity
and high temperature, then the gas can expand relatively easily. When the magma
reaches the surface, the gas will easily expand and a non-explosive eruption
will occur, usually as a lava flow (Lava is the name we
give to magma on the surface of the Earth).
(b) Volcanic dome
Volcanic Domes result from the extrusion of highly
viscous, gas poor andesitic and rhyolitic lava. Since the viscosity is so high,
the lava does not flow away from the vent, but instead piles up over the vent
3-
Compare between the following:
|
Mid Oceanic Ridges
|
Volcanic arc
|
1- Rock types
|
Mainly basalts (massive, pillow)
and gabbros
|
Minor basalts, mainly andesites,
dacites, rhyolites and their plutonic equivalents
|
2- Tectonic Setting
|
Divergent plate boundaries
|
Convergent plate boundaries
|
3- Magma type
|
Mainly tholeiitic
|
Calc-alkaline, Tholeiitic and
alkaline
|
4- Main Geochemical
characteristics
|
MORBs
appear to be the result of melting of an incompatible element depleted
mantle, both in terms of their incompatible trace element compositions and
isotopic ratios of Sr and Nd.
|
Enriched in LILE snd depleted in
HFSE. The hydrous fluids carry with them high concentrations of LILE and REE,
but leave behind the relatively insoluble HFSE. They also carry the isotopic
signature of the basaltic crust sediment mixture that released the fluids,
and thus have higher 87Sr/86Sr ratios and lower 143Nd/144Nd
ratios,
|
4-
Compare between the following:
|
S-type granites
|
I-type granites
|
1- Characteristic
minerals
|
commonly muscovite, although other minerals such
as the Al2SiO5 minerals and corundum may also occur
|
contain biotite and hornblende as the major mafic
minerals.
|
2- Tectonic Setting
|
fold-thrust mountain belts formed as a result of
continent-continent collisions
|
continental margins
|
3- Magma type
|
peraluminous granites [Al2O3
> (Na2O + K2O+CaO)
|
These are generally metaluminous granites
|
5- Describe the different ways
to melt a rock, Illustrate your answer by labeled drawings and give an example
for each.
1- Decompression:
Decompression melting occurs at mid-ocean ridges
2- Addition of Fluxes: Rocks melt at a lower
temperature in the presence of volatiles, such as water and carbon dioxide. How
do you get water underneath a volcano? The most common way to do it is to send
it down a subduction zone.
3- Rising temperature: The third way to melt a rock
is by conduction. Conduction is the simplest way to transfer heat.
6- Name 5 processes that might
cause the chemical composition of magma to change.
1- Partial melting (to produce different magmas)
2- Crystal fractionation
3- Liquid immiscibility
4- Magma mixing
5- Assimilation
7-
What kind of evidence one look for to determine if crustal assimilation has
operated to change the composition of magma.
Criteria
for recognition of assimilation:
1- The
occurrence of xenoliths in the igneous rocks, which are of similar composition
to the intruded country rocks.
2- Disequilibrium
mineral assemblage and Resorbed xenocrysts.
3- On
variation diagrams, the composition of the igneous rock after assimilation lies
on a mixing (straight) line between its composition prior to assimilation and
the composition of the assimilated rock.
4- “Higher”
87Sr/86Sr and 18O values (as will be
discussed later).
8-
The following diagram represents the REE patterns for 4 melts (a, b, c, and d)
derived by different degrees of partial melting of a mantle source. Which melt
represent the lower degree of partial melting and why?
Pattern d represent the lower degree of partial melting
This is because the LREE are incompatible elements
(Elements prefer to be present in the melt) and their contents will become less
as the degree of partial melting increase.
9-
The following Table shows the partition coefficient (KD) values for
Ni in the listed minerals.
a- Define partition
coefficient (KD)
The
partition
coefficient is a
ratio of concentrations of an element between
crystalline solids and coexisting liquid phases. Kd= Conc. of element in
solid/conc. Of element in liquid
b- Calculate the
bulk partition coefficient (D) for Ni in garnet lherzolite containing 60%
olivine, 25% orthopyroxene, 10% clinopyroxene and 5% garnet.
Bulk KdNi=(0.6*14)+(0.25*5)+(0.1*7)+(0.0995*0.05)=
10.35
|
Olivine
|
Orthopyroxene
|
Clinopyroxene
|
Garnet
|
Ni
|
14
|
5
|
7
|
0.955
|
10-
Complete the following Table for pyroclastic classification.
Average Particle Size (mm)
|
Unconsolidated Material (Tephra)
|
Pyroclastic Rock
|
>64
|
Bombs or Blocks
|
Agglomerate
|
2 - 64
|
Lapilli
|
Lapilli Tuff
|
<2
|
Ash
|
Ash Tuff
|
11-
Compare between the different types of magmas according to the following table:
Magma Type
|
Chemical Composition
|
Temperature
|
Viscosity
|
Gas Content
|
Basaltic
|
45-55 SiO2
%, high in Fe, Mg, Ca, low in K, Na
|
1000 - 1200 oC
|
Low
|
Low
|
Andesitic
|
55-65 SiO2
%, intermediate in Fe, Mg, Ca, Na, K
|
800 - 1000 oC
|
Intermediate
|
Intermediate
|
Rhyolitic
|
65-75 SiO2
%, low in Fe, Mg, Ca, high in K, Na.
|
650 - 800 oC
|
High
|
High
|
12- Complete
the following Table as the given example:
Rock Name
|
Occurrence
|
Characteristic
minerals
|
Chemical
classification
|
Basalt
|
Volcanic
(extrusive)
|
Pyroxene + calcic
plagioclase± olivine
|
Mafic
|
Rhyolite
|
Volcanic
|
Plagioclase + K-feldspar + Quartz ± Mica
|
Acidic
|
Peridotite
|
Plutonic
|
Olivine + pyroxene
|
Ultra-mafic
|
Granodiorite
|
Plutonic
|
Plagioclase + quartz + k-feldspar + mica
+ Amphibole
|
Acidic
|
Gabbro
|
Plutonic
|
Plagioclase + ortho-pyroxene ± olivine
|
Mafic
|
|