Sedimentary Petrology
Go to: Final Exam
The following quiz assumes that you have the background knowledge from GLGY 491. For additional questions specific to organisms, please check Geology 491 materials. Most concepts related to 491 class has been omitted from this quiz.
Attention: Application questions
Please be aware that you may come across difficult questions. They are usually not directly from one particular lecture but rather application of principles form several different lectures and labs. In this particular class, you are expected to solve this type of questions for the lecture/lab midterms and the finals. It is not my intention to make this quiz questions hard like a jackass.
Geology (GLGY 461-UCAL) Midterm
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Question 1 |
A | Platform slopes |
B | Outer platform margin biostromes |
C | Shallow internal platform biostromes |
D | Open-water supertidal flats |
E | Open-water mud mounds |
Question 2 |
A | Siliciclastic mudstones |
B | Halites |
C | Siliciclastic sandstones |
D | Phosphorites |
E | Limestones |
F | Dolostones |
Question 3 |
A | A. colonial B. solitary |
B | A. calcitic B. siliceous |
C | A. aragonitic B. calcitic |
D | A. calcitic B. aragonitic |
E | A. siliceous B. calcitic |
Question 4 |
A | True |
B | False, they were found in laminae, pillars and astrorhizae forms. |
C | False, they were found in mounded laminae forms. |
Question 5 |
A | No, it is a synthetic material. |
B | Yes it is a mineral. |
C | No, it is only the chemical formula for a mineral. |
D | No, it is neither a mineral nor a valid chemical formula. |
Question 6 |
A | The process in which constituents were transported from the initial deposition location to a basin for burial. |
B | The process in which constituents were combined to form metamorphic rocks. |
C | The process in which constituents were broken down during the burial to form new minerals in the sediment. |
D | The process in which rocks were cooled down after a burial process to from new rocks. |
Question 7 |
A | Brachiopods |
B | Molluscs |
C | Foraminifera |
D | Echinoderms |
Question 8 |
A | Rudstones |
B | Bindstones |
C | Bafflestones |
D | Floatstones |
E | Framestones |
Question 9 |
A | Multiple chemical elements within growth lines |
B | Foliation |
C | Double-crystal system |
D | Cross-lamellar |
Question 10 |
A | Foliation grade differences during each growth cycle. |
B | Overlap of 1-st and 2-nd Order lamellae. |
C | Longitudinal deformation due to stresses during sedimentation. |
D | Changes in chemical composition during each growth cycle. |
E | Due to their orientation to the cut surface of the thin section. |
Question 11 |
A | Single crystal structures |
B | Composite prismatic structures |
C | Foliated structures |
D | Fascicular fibrous structures |
Question 12 |
A | True |
B | False |
Question 13 |
A | Pattern of the cross; the 1-st Order structures V-shaped. |
B | Pore/void space: the 1-st Order structures have less void space. |
C | Pattern of the cross; the 2-st Order structures V-shaped. |
D | Shape and size; the 2-st Order structures are larger. |
E | Pore/void space: the 2-st Order structures have less void space. |
F | Shape and size; the 1-st Order structures are larger. |
Question 14 |
A | Several layers of complex and composite prismatic structures. Hint: Nope; this is for molluscus ONLY. |
B | Homogeneous prismatic structures with no deformation. Hint: Nope; this is mostly for forminifera and molluscs. |
C | Several layers of foliated or normal prismatic structures. |
D | At lest two layers with 1-st and 2-nd Order aragonitic crossed-lamellar layers. Hint: Nope; this is for molluscus. |
E | At least two layers of non-deformed single crystal structures. Hint: Nope; this is mostly for echinoderms. |
Question 15 |
A | Change in temperature only. |
B | Change in the rate at which the burial of sediments occurs. |
C | Change in temperature and pressure. |
D | Change in abundance of organisms in a macro-region. |
E | Change in abundance of chemicals. |
F | Change in abundance of organisms in a micro-region. |
Question 16 |
A | Outer platform margin bioherms |
B | Platform slopes |
C | Supertidal flats |
D | Shallow internal platform biostromes |
E | Open-water mud mounds |
Question 17 |
A | It was first published in 1975 by Wilson. |
B | It dose not consider effects of sea level changes or climate controls. |
C | It is an ideal model of platform environment that will work for most areas of Earth. |
D | It is often used for pleobilogical stratigraphic analysis. |
Question 18 |
A | Nature of the tidal flat, lagoonal faces, shallow ramp and deep shelf ramp. |
B | Variations in the global biological and lithological diversity. |
C | Common lithofacies. |
D | Common lithofacies and biological characteristics. |
E | Depositional setting, sediment type, biota and common lithofacies. |
Question 19 |
A | I. Hermatypic II. Ahermatypic |
B | I. Ahermatypic II. Hermatypic |
C | I. Brain II. Hexacorallia Hint: Both are reef builders. |
D | I. Hexacorallia II. Brain Hint: Both are reef builders. |
E | I. Rugose II. Brain |
Question 20 |
A | Around 300 m |
B | Between 200 m and 300 m |
C | Between 150 m and 200 m |
D | Below 100 m |
E | Around 200 m |
Question 21 |
A | True |
B | False; they are an extinct class of organisms. |
C | False; they are solitary organisms. |
Question 22 |
A | Deep Tidal Flat Facies |
B | Lagoonal Facies |
C | Deep Basin Facies |
D | Shallow Ramp Facies |
E | Deep Shelf Facies |
Question 23 |
A | low energy reef/ramp environments. |
B | high energy slope environments. |
C | low energy shallow tidal environments. |
D | high energy deep tidal environments. |
Question 24 |
A | Alteration of grains |
B | Reworked lithofied clasts |
C | In-situ formation |
D | Biotic |
Question 25 |
A | Large volume of spherical/sub-spherical shaped peloids. |
B | Large pour spaces caused by entrapment of gaseous substance. |
C | Large volume of elongated peloids. |
D | Presence of destructive micritization. |
E | Presence of bio-chemicals and organic matter. |
Question 26 |
A | high global biological activities due to abundance in nutrients. Hint: Think again; usually "abundance of peloidal rocks" found in specific areas in specific geologic time. |
B | very high energy environment. |
C | very low energy environment. |
D | high local biological activities due to abundance in nutrients. |
E | Presence of biotic peloids as opposed to other types. |
Question 27 |
A | False; because it is an indication of reworked lithofied clasts of carbonates origin. |
B | True |
C | False; because it is an indication of altered grains forming micritized peloids. |
D | False; because it is an indication of in-situ formations. |
Question 28 |
A | cyanobacterial destruction. |
B | constructive micritization. |
C | destructive micritization. |
D | microborings. |
Question 29 |
A | Ooids with very thin cortex. |
B | Ooids with very thick cortex. |
C | Thin cortex very thin cortex and 1-3 counted layers. |
D | Thin cortex very thick cortex and innumerable layers. |
E | Thin cortex very thin cortex and 2-4 counted layers. |
Question 30 |
A | Usually have a nuclei. |
B | Bottom agitation, presence of nuclei and grain degradation. |
C | Presence of nuclei and undersaturated water with respect to calcite. |
D | Presence of nuclei and supersaturated water with respect to calcite. |
Question 31 |
A | at the asymmetric surfaces. |
B | along the troughs of parabolic bars. |
C | at the trough of the dunes. |
D | at the peak of the crest (peak) of the dunes. |
E | at the points of flow convergence. |
Question 32 |
A | Green algae are adapted to deeper water environments and they absorbs red light. |
B | Red algae are adapted to deeper water environments and they absorbs red light. |
C | Red algae are adapted to deeper water environments and they absorbs blue light. |
D | Green algae are adapted to deeper water environments and they absorbs blue light. |
E | Blue algae are adapted to deeper water environments and they absorbs blue light. |
F | Blue algae are adapted to deeper water environments and they absorbs red light. |
G | Green algae are adapted to shallow water environments and they absorbs yellow light. |
Question 33 |
A | ...adapted to deep water environments. |
B | ...were exclusive to fresh water environments during Carboniferous and modern day they are exclusive to marine water environments. |
C | ...most abundant in shallow, protected environments. |
D | ...exclusive to fresh water environments. |
E | ....exclusive to marine water environments. |
Question 34 |
A | Red |
B | Green |
C | All types (Green, Blue and Red) |
D | Blue |
Question 35 |
A | They can be in several depositional settings such as marine, fresh-brackish water ponds, tidal flats and shallow sandy bottoms. |
B | They are important sediment produces and reef builders. |
C | They are very important for economic resources such as diamond and gold ores. |
D | Some of them are capable of secreting or depositing carbonate around their body. |
E | This group includes both benthic and planktonic organisms that have the ability to photosynthesize. |
Question 36 |
A | Chlorophyta |
B | Rhodophyta |
C | Cynaophyta |
D | Chrysophyta |
Question 37 |
A | Green algae |
B | Blue algae |
C | Yellow algae |
D | Red algae |
Question 38 |
A | Tidal flats |
B | Restricted marine bays and lagoons |
C | Reef fronts |
D | Open marines |
E | Open marine bay shelf lagoons |
Question 39 |
A | I. spinal core II. external core |
B | I. medulla II. cortex |
C | I. cortex II. medulla |
D | I. central core II. outer core |
Question 40 |
A | Ediacaran |
B | Cenozoic |
C | Cretaceous |
D | Paleozoic |
E | Carboniferous |
Question 41 |
A | Sunlight and moisture |
B | Sunlight and high energy water currents |
C | Sunlight and availability of calcareous fluids |
D | High energy water currents |
E | Sunlight |
Question 42 |
A | CCD or carbon compensation depth is the depth in which the calcite start to become unstable. Hint: Nope; that would be Lysoclines |
B | Large portion of the mixing zone is in the marine diagenetic area. |
C | Sediments could undergo marine diagenesis as long as water is present. |
D | The best cementation processes occurs at shallow waters such as at the shelf or slopes. |
E | The partial pressure of CO2 is very high at shallow depths; leads to good cementation. |
Question 43 |
A | I. Yellow II. green |
B | I. Green
II. red |
C | I. Blue II. green |
D | I. Red II. green |
Question 44 |
A | layering. |
B | zoecias. |
C | pillars. |
D | alternating sediment-organic matter layers. |
E | lamination. |
Question 45 |
A | True |
B | False |
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Credits: Based on the excellent class notes provided by, Dr. Rudi Meyer during Winter 2014.
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