بنك الاسئلة EMR 2010 2ND SEMESTER 421


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

 


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8/20/2012 7:32:49 PM