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 | Shallow internal platform biostromes |
B | Outer platform margin biostromes |
C | Open-water supertidal flats |
D | Open-water mud mounds |
E | Platform slopes |
Question 2 |
A | Siliciclastic sandstones |
B | Limestones |
C | Siliciclastic mudstones |
D | Dolostones |
E | Phosphorites |
F | Halites |
Question 3 |
A | A. siliceous B. calcitic |
B | A. calcitic B. siliceous |
C | A. colonial B. solitary |
D | A. calcitic B. aragonitic |
E | A. aragonitic B. calcitic |
Question 4 |
A | False, they were found in laminae, pillars and astrorhizae forms. |
B | False, they were found in mounded laminae forms. |
C | True |
Question 5 |
A | Yes it is a mineral. |
B | No, it is a synthetic material. |
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 broken down during the burial to form new minerals in the sediment. |
B | The process in which rocks were cooled down after a burial process to from new rocks. |
C | The process in which constituents were combined to form metamorphic rocks. |
D | The process in which constituents were transported from the initial deposition location to a basin for burial. |
Question 7 |
A | Foraminifera |
B | Brachiopods |
C | Molluscs |
D | Echinoderms |
Question 8 |
A | Rudstones |
B | Framestones |
C | Bindstones |
D | Bafflestones |
E | Floatstones |
Question 9 |
A | Multiple chemical elements within growth lines |
B | Cross-lamellar |
C | Double-crystal system |
D | Foliation |
Question 10 |
A | Changes in chemical composition during each growth cycle. |
B | Overlap of 1-st and 2-nd Order lamellae. |
C | Foliation grade differences during each growth cycle. |
D | Longitudinal deformation due to stresses during sedimentation. |
E | Due to their orientation to the cut surface of the thin section. |
Question 11 |
A | Foliated structures |
B | Single crystal structures |
C | Composite prismatic structures |
D | Fascicular fibrous structures |
Question 12 |
A | False |
B | True |
Question 13 |
A | Pore/void space: the 1-st Order structures have less void space. |
B | Pattern of the cross; the 1-st Order structures V-shaped. |
C | Pattern of the cross; the 2-st Order structures V-shaped. |
D | Pore/void space: the 2-st Order structures have less void space. |
E | Shape and size; the 2-st Order structures are larger. |
F | Shape and size; the 1-st Order structures are larger. |
Question 14 |
A | Several layers of foliated or normal prismatic structures. |
B | At lest two layers with 1-st and 2-nd Order aragonitic crossed-lamellar layers. Hint: Nope; this is for molluscus. |
C | Several layers of complex and composite prismatic structures. Hint: Nope; this is for molluscus ONLY. |
D | Homogeneous prismatic structures with no deformation. Hint: Nope; this is mostly for forminifera and molluscs. |
E | At least two layers of non-deformed single crystal structures. Hint: Nope; this is mostly for echinoderms. |
Question 15 |
A | Change in abundance of chemicals. |
B | Change in abundance of organisms in a micro-region. |
C | Change in abundance of organisms in a macro-region. |
D | Change in temperature and pressure. |
E | Change in the rate at which the burial of sediments occurs. |
F | Change in temperature only. |
Question 16 |
A | Outer platform margin bioherms |
B | Platform slopes |
C | Open-water mud mounds |
D | Supertidal flats |
E | Shallow internal platform biostromes |
Question 17 |
A | It dose not consider effects of sea level changes or climate controls. |
B | It is an ideal model of platform environment that will work for most areas of Earth. |
C | It was first published in 1975 by Wilson. |
D | It is often used for pleobilogical stratigraphic analysis. |
Question 18 |
A | Common lithofacies. |
B | Depositional setting, sediment type, biota and common lithofacies. |
C | Variations in the global biological and lithological diversity. |
D | Common lithofacies and biological characteristics. |
E | Nature of the tidal flat, lagoonal faces, shallow ramp and deep shelf ramp. |
Question 19 |
A | I. Ahermatypic II. Hermatypic |
B | I. Rugose II. Brain |
C | I. Hexacorallia II. Brain Hint: Both are reef builders. |
D | I. Brain II. Hexacorallia Hint: Both are reef builders. |
E | I. Hermatypic II. Ahermatypic |
Question 20 |
A | Below 100 m |
B | Between 200 m and 300 m |
C | Around 300 m |
D | Around 200 m |
E | Between 150 m and 200 m |
Question 21 |
A | True |
B | False; they are solitary organisms. |
C | False; they are an extinct class of organisms. |
Question 22 |
A | Deep Tidal Flat Facies |
B | Shallow Ramp Facies |
C | Deep Basin Facies |
D | Deep Shelf Facies |
E | Lagoonal Facies |
Question 23 |
A | low energy shallow tidal environments. |
B | high energy slope environments. |
C | high energy deep tidal environments. |
D | low energy reef/ramp environments. |
Question 24 |
A | Biotic |
B | Alteration of grains |
C | Reworked lithofied clasts |
D | In-situ formation |
Question 25 |
A | Large pour spaces caused by entrapment of gaseous substance. |
B | Large volume of spherical/sub-spherical shaped peloids. |
C | Presence of bio-chemicals and organic matter. |
D | Large volume of elongated peloids. |
E | Presence of destructive micritization. |
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 | Presence of biotic peloids as opposed to other types. |
D | high local biological activities due to abundance in nutrients. |
E | very low energy environment. |
Question 27 |
A | False; because it is an indication of reworked lithofied clasts of carbonates origin. |
B | False; because it is an indication of altered grains forming micritized peloids. |
C | True |
D | False; because it is an indication of in-situ formations. |
Question 28 |
A | cyanobacterial destruction. |
B | destructive micritization. |
C | microborings. |
D | constructive micritization. |
Question 29 |
A | Thin cortex very thick cortex and innumerable layers. |
B | Thin cortex very thin cortex and 1-3 counted layers. |
C | Ooids with very thin cortex. |
D | Ooids with very thick cortex. |
E | Thin cortex very thin cortex and 2-4 counted layers. |
Question 30 |
A | Usually have a nuclei. |
B | Presence of nuclei and supersaturated water with respect to calcite. |
C | Presence of nuclei and undersaturated water with respect to calcite. |
D | Bottom agitation, presence of nuclei and grain degradation. |
Question 31 |
A | at the points of flow convergence. |
B | at the asymmetric surfaces. |
C | at the trough of the dunes. |
D | at the peak of the crest (peak) of the dunes. |
E | along the troughs of parabolic bars. |
Question 32 |
A | Red algae are adapted to deeper water environments and they absorbs blue light. |
B | Green algae are adapted to shallow water environments and they absorbs yellow light. |
C | Red algae are adapted to deeper water environments and they absorbs red light. |
D | Blue algae are adapted to deeper water environments and they absorbs blue light. |
E | Blue algae are adapted to deeper water environments and they absorbs red light. |
F | Green algae are adapted to deeper water environments and they absorbs red light. |
G | Green algae are adapted to deeper water environments and they absorbs blue light. |
Question 33 |
A | ....exclusive to marine water environments. |
B | ...exclusive to fresh water environments. |
C | ...adapted to deep water environments. |
D | ...were exclusive to fresh water environments during Carboniferous and modern day they are exclusive to marine water environments. |
E | ...most abundant in shallow, protected environments. |
Question 34 |
A | All types (Green, Blue and Red) |
B | Blue |
C | Red |
D | Green |
Question 35 |
A | This group includes both benthic and planktonic organisms that have the ability to photosynthesize. |
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 | They can be in several depositional settings such as marine, fresh-brackish water ponds, tidal flats and shallow sandy bottoms. |
Question 36 |
A | Rhodophyta |
B | Chrysophyta |
C | Cynaophyta |
D | Chlorophyta |
Question 37 |
A | Blue algae |
B | Red algae |
C | Green algae |
D | Yellow algae |
Question 38 |
A | Restricted marine bays and lagoons |
B | Reef fronts |
C | Open marine bay shelf lagoons |
D | Open marines |
E | Tidal flats |
Question 39 |
A | I. spinal core II. external core |
B | I. cortex II. medulla |
C | I. medulla II. cortex |
D | I. central core II. outer core |
Question 40 |
A | Ediacaran |
B | Carboniferous |
C | Cretaceous |
D | Cenozoic |
E | Paleozoic |
Question 41 |
A | Sunlight and availability of calcareous fluids |
B | High energy water currents |
C | Sunlight and moisture |
D | Sunlight and high energy water currents |
E | Sunlight |
Question 42 |
A | Sediments could undergo marine diagenesis as long as water is present. |
B | CCD or carbon compensation depth is the depth in which the calcite start to become unstable. Hint: Nope; that would be Lysoclines |
C | The partial pressure of CO2 is very high at shallow depths; leads to good cementation. |
D | The best cementation processes occurs at shallow waters such as at the shelf or slopes. |
E | Large portion of the mixing zone is in the marine diagenetic area. |
Question 43 |
A | I. Blue II. green |
B | I. Red II. green |
C | I. Green
II. red |
D | I. Yellow II. green |
Question 44 |
A | layering. |
B | zoecias. |
C | pillars. |
D | alternating sediment-organic matter layers. |
E | lamination. |
Question 45 |
A | False |
B | True |
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Credits: Based on the excellent class notes provided by, Dr. Rudi Meyer during Winter 2014.
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