Igneous Petrology
This is an “extension” of Geology 311 (Mineralogy and Rocks) at the University of Calgary. The foundation for these two particular subjects can be found in Geology 311 Midterm and Geology 311 Final pages. Other 300 and 400-level classes such as Structural Geology and Advanced Mineralogy will also help you out. On this page, ONLY the advanced materials are empathized because I do not think it is productive to repeat information from junior classes. Visit this page for Metamorphic Petrology
Geology (GLGY 443-UCAL) Midterm
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Question 1 |
A | Slow rate crystallization. |
B | Sudden increase in temperature. |
C | Gradual increase in temperature. |
D | Increase in pressure. |
E | Removal of volatiles. |
Question 2 |
A | Change in the state of the material from gas to liquid or vice versa. |
B | Change in the chemical composition of the magma due to magma mixing from another source. |
C | Decrease in pressure and increased in temperature. |
D | Addition of volatiles to the magma by hydrous minerals. |
Question 3 |
A | 4 |
B | 7 |
C | 6 |
D | 5 |
E | 3 |
Question 4 |
A | density of the whole rock |
B | radio active dating |
C | chemical composition variations |
D | volumetric proportions of minerals |
E | x-ray analysis |
Question 5 |
A | Werners and Abrahams |
B | Chills and Hards |
C | Neptunist and Plutonists |
D | Werners and Huttons |
Question 6 |
A | The stresses (forces) are either two weak or non-existent in igneous environments. |
B | The isotopic chemical configurations would not allow foliation to be formed in igneous rocks. Hint: Dude, WTF? This won't even make sense! |
C | The liquid nature of igneous rocks cannot sustain substantial directional stressed. |
D | The crystals has been already formed by the time igneous rocks undergo change in directional forces. |
Question 7 |
A | Liquid Immiscibility |
B | Thermogravitational Diffusion |
C | Magma Mixing |
D | Assimilation |
E | Fractional Crystallization |
Question 8 |
A | I. 66 II. ultrabasic |
B | I. 45 II. intermediate |
C | I. 45 II. basic |
D | I. 66 II. acidic |
Question 9 |
A | Outer core |
B | D-layer |
C | Inner core |
D | Upper layer |
Question 10 |
A | By using the Birefringence difference between each rim. |
B | By using the Reflective Indexes (Becke line test) |
C | By using the XRF or in situ chemical analysis. |
D | By adding a dye to a thin section and analyzing the variation in the intensity of colours. |
Question 11 |
A | incongruent melting |
B | Dry solid melting |
C | solid solution melting |
D | congruent melting |
E | Wet solid melting |
Question 12 |
A | This particular rock sample was formed in a volcanic environment. |
B | This particular rock sample was formed from a silica under saturated magma. |
C | This particular rock sample was formed in a plutonic environment. |
D | This particular rock sample was formed from a silica over saturated magma. |
E | This particular rock sample was formed from an ultra mafic magma. |
F | This particular rock sample was formed from a purely silica based magma. |
Question 13 |
A | chadacryst |
B | mound |
C | oikocryst |
D | poikili |
E | cumulate |
Question 14 |
A | The leakage of water from above (the melting locale) due to surface and groundwater runoff. |
B | Dehydration of rocks due to the rapid decompression at the melting locale (location). |
C | The dehydration of minerals below the melting locale (location). |
D | Addition of water through the oceans in Mid Ocean Ridges. |
E | The dehydration of rocks above the melting locale (location). |
Question 15 |
A | ~ 40 - 50 % |
B | ~ 70 - 80 % |
C | ~ 90 - 99 % (almost all of it) |
D | ~ 15 - 20 % |
E | 0 % (none) |
Question 16 |
A | True |
B | False; it depends on the magma temperature. |
C | False; it depends on the amount of hydrous minerals in the magma. |
Question 17 |
A | phaneritic rock |
B | peloidal rock |
C | large grained rock |
D | aphanitic rock |
Question 18 |
A | Passive gravity |
B | Variations in temperature within a magma |
C | Density variations |
D | Geothermal gradient |
E | Pressure variations |
Question 19 |
A | Spinifex flow |
B | Grass flow |
C | Volcanic mud flow |
D | Komatiite flow |
E | Pyroclastic flow |
Question 20 |
A | False; only on rocks that has no hydrous minerals in the original melt. |
B | True |
C | False; only on rock samples that crystallized at shallow low pressure environments. |
D | False; only on rocks that formed in volcanic environments. |
Question 21 |
A | Cumulative zones |
B | Chilled margins |
C | Platy-spinifex area |
D | Random-spinifex area |
Question 22 |
A | ...a measurement which can be calculated using mole fractions of solids and liquids in a magma. |
B | ...the ability for materials to flow. |
C | ..,a property that is directly related to density of the material. |
D | ...a property that only applicable to 100% pure liquids. |
E | ...the ability of materials to resist shear stress (forces). |
Question 23 |
A | Contains very high percentage of plagioclase feldspars. |
B | All rocks that contains over 70% of mafic minerals are ultramafic rocks. Hint: Nope; must be over 90% |
C | Contains no plagioclase feldspars. |
D | They are mostly associated with pyroclastic materials. |
E | They are highly rich in quartzs and quartzites. |
Question 24 |
A | Olivine |
B | Websterite |
C | Lherzolite |
D | Precipitates |
E | Pyroxenes (ortho/clino) |
Question 25 |
A | True |
B | False |
Question 26 |
A | It is the process of cooling a magma below the parental temperature but still maintain the temperature above the melting point. |
B | It is the process of cooling a magma below the melting point without producing crystals. |
C | It is the process of cooling a magma below the melting point by forming crystals. |
D | It is a magmatic process in which inhibits crystal formation completely. |
Question 27 |
A | True |
B | False |
Question 28 |
A | Radiation of energy out of a undefined nucleus. |
B | Addition of chemical materials. |
C | Differentiation of ions. |
D | Release of ions from the nucleus. |
E | Nucleation of embryos of crystals. |
Question 29 |
A | I. higher II. increase |
B | I. lower II. decrease |
C | I. lower II. increase |
D | I. higher II. decrease |
Question 30 |
A | I. solid rocks II. crust |
B | I. outer core II. mantle |
C | I. mantle II. crust |
D | I. crust II. mantle |
E | I. solid rocks II. mantle |
Question 31 |
A | All solids at low pressure will melt at low temperature. |
B | All solids will eventually turns to liquids at high temperature. |
C | Solidus and liquidus varies with material composition. Hint: True; but that's not what this equation proving. |
D | Dry materials have a lower temperature solidus. Hint: True; but that's not what this equation proving. |
Question 32 |
A | The rock must have a plutonic origin. |
B | All silica weight percentages were taken out from the analysis. |
C | The rock must have a volcanic or pyroclastic flow origin. |
D | Hydrous minerals are taken out from the analysis. |
E | The rock must have a mafic origin. |
Question 33 |
A | Caused by mixing of magma from two or more (different) sources. |
B | A difference in chemical structure but with the exact same chemical formula. |
C | Growth of a new mineral by replacing another with the shape of the original mineral. |
D | Growth of a secondary mineral as a result of hydrothermal fluids. |
E | A condition in which a mineral exhibit of properties of another (hence making identification impossible). |
Question 34 |
A | I. high-energy II. low-energy |
B | I. homogeneous II. heterogeneous |
C | I. epithermal II. thermal |
D | I. low-energy II. high-energy |
E | I. heterogeneous II. homogeneous |
F | I. thermal II. epithermal |
Question 35 |
A | Rhyolitic magma |
B | Andesitic magma |
C | Basaltic magma |
D | Magmas with very high water content |
Question 36 |
A | secondary |
B | tertiary |
C | primary |
D | quaternary |
Question 37 |
A | glass. |
B | ions. |
C | large number of small crystals. |
D | random nuclei. |
E | small number of large crystals. |
Question 38 |
A | The volatiles are in free form. |
B | The volatiles are always ionically bonded. |
C | The volatiles cannot be released unless the pressure is decreased. Hint: Nope; it is opposite. The pressure increase will result in the release of volatiles. |
D | The volatiles are always in the form of pure water. |
E | The volatiles are in the saturated form. |
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You may download this exam as a PDF file here.
Credits: Based on the excellent class notes provided by, Igneous: Dr. Rajeev Nair and Metamorphic: Dr. David Pattison during Winter 2014.
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Also visit: Petrology Media Library
List of concepts
Igneous Petrology
- Formation of igneous rocks and their compositional variations.
- Difference between MORB and OIB basalts.
- Difference between mafic and felsic magma (and processes).
- Magma differentiation and layered mafic intrusions.
- Physical and chemical properties
- Geochemical processes (magma differentiation, isotopic variations, melting and cooling, etc), phase equilibria and geothermobarometry
- Classifications and textures.
- Other processes such as island arcs and continental flood basalts.
Metamorphic Petrology
- What are metamorphic rocks and how do they differ from igneous and sedimentary rocks?
- What is petrology?
- Differences between stress, strain and pressure dynamics.
- Hydrostatic and lithostatic pressures and the orientations of sigma-1,2,3.
- Difference between lineation of foliation.
- Metamorphic textures and structures; deformation, P-T driven textural changes, grain size and shape, grading (graded beds/layers), inclusions, etc.
- History and current condition of rocks.
- Classifications and textures.