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 mud mounds |
E | Open-water supertidal flats |
Question 2 |
A | Siliciclastic mudstones |
B | Halites |
C | Phosphorites |
D | Limestones |
E | Siliciclastic sandstones |
F | Dolostones |
Question 3 |
A | A. aragonitic B. calcitic |
B | A. colonial B. solitary |
C | A. siliceous B. calcitic |
D | A. calcitic B. aragonitic |
E | A. calcitic B. siliceous |
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 | No, it is only the chemical formula for a mineral. |
C | Yes it is 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 rocks were cooled down after a burial process to from new 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 constituents were combined to form metamorphic rocks. |
Question 7 |
A | Foraminifera |
B | Brachiopods |
C | Echinoderms |
D | Molluscs |
Question 8 |
A | Framestones |
B | Floatstones |
C | Rudstones |
D | Bafflestones |
E | Bindstones |
Question 9 |
A | Foliation |
B | Cross-lamellar |
C | Double-crystal system |
D | Multiple chemical elements within growth lines |
Question 10 |
A | Longitudinal deformation due to stresses during sedimentation. |
B | Overlap of 1-st and 2-nd Order lamellae. |
C | Changes in chemical composition during each growth cycle. |
D | Foliation grade differences during each growth cycle. |
E | Due to their orientation to the cut surface of the thin section. |
Question 11 |
A | Fascicular fibrous structures |
B | Composite prismatic structures |
C | Single crystal structures |
D | Foliated structures |
Question 12 |
A | False |
B | True |
Question 13 |
A | Pattern of the cross; the 2-st Order structures V-shaped. |
B | Pore/void space: the 2-st Order structures have less void space. |
C | Shape and size; the 1-st Order structures are larger. |
D | Pattern of the cross; the 1-st Order structures V-shaped. |
E | Shape and size; the 2-st Order structures are larger. |
F | Pore/void space: the 1-st Order structures have less void space. |
Question 14 |
A | At lest two layers with 1-st and 2-nd Order aragonitic crossed-lamellar layers. Hint: Nope; this is for molluscus. |
B | Several layers of complex and composite prismatic structures. Hint: Nope; this is for molluscus ONLY. |
C | At least two layers of non-deformed single crystal structures. Hint: Nope; this is mostly for echinoderms. |
D | Several layers of foliated or normal prismatic structures. |
E | Homogeneous prismatic structures with no deformation. Hint: Nope; this is mostly for forminifera and molluscs. |
Question 15 |
A | Change in abundance of organisms in a macro-region. |
B | Change in abundance of organisms in a micro-region. |
C | Change in temperature and pressure. |
D | Change in abundance of chemicals. |
E | Change in the rate at which the burial of sediments occurs. |
F | Change in temperature only. |
Question 16 |
A | Shallow internal platform biostromes |
B | Supertidal flats |
C | Platform slopes |
D | Open-water mud mounds |
E | Outer platform margin bioherms |
Question 17 |
A | It is an ideal model of platform environment that will work for most areas of Earth. |
B | It dose not consider effects of sea level changes or climate controls. |
C | It is often used for pleobilogical stratigraphic analysis. |
D | It was first published in 1975 by Wilson. |
Question 18 |
A | Common lithofacies. |
B | Nature of the tidal flat, lagoonal faces, shallow ramp and deep shelf ramp. |
C | Depositional setting, sediment type, biota and common lithofacies. |
D | Variations in the global biological and lithological diversity. |
E | Common lithofacies and biological characteristics. |
Question 19 |
A | I. Ahermatypic II. Hermatypic |
B | I. Hexacorallia II. Brain Hint: Both are reef builders. |
C | I. Brain II. Hexacorallia Hint: Both are reef builders. |
D | I. Hermatypic II. Ahermatypic |
E | I. Rugose II. Brain |
Question 20 |
A | Around 300 m |
B | Between 150 m and 200 m |
C | Below 100 m |
D | Between 200 m and 300 m |
E | Around 200 m |
Question 21 |
A | False; they are an extinct class of organisms. |
B | True |
C | False; they are solitary organisms. |
Question 22 |
A | Deep Shelf Facies |
B | Deep Basin Facies |
C | Lagoonal Facies |
D | Deep Tidal Flat Facies |
E | Shallow Ramp Facies |
Question 23 |
A | low energy reef/ramp environments. |
B | low energy shallow tidal environments. |
C | high energy deep tidal environments. |
D | high energy slope environments. |
Question 24 |
A | In-situ formation |
B | Biotic |
C | Alteration of grains |
D | Reworked lithofied clasts |
Question 25 |
A | Large volume of spherical/sub-spherical shaped peloids. |
B | Presence of bio-chemicals and organic matter. |
C | Large volume of elongated peloids. |
D | Presence of destructive micritization. |
E | Large pour spaces caused by entrapment of gaseous substance. |
Question 26 |
A | very high energy environment. |
B | very low energy environment. |
C | Presence of biotic peloids as opposed to other types. |
D | high local biological activities due to abundance in nutrients. |
E | 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. |
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 | False; because it is an indication of in-situ formations. |
D | True |
Question 28 |
A | cyanobacterial destruction. |
B | microborings. |
C | constructive micritization. |
D | destructive 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 | Bottom agitation, presence of nuclei and grain degradation. |
B | Presence of nuclei and supersaturated water with respect to calcite. |
C | Usually have a nuclei. |
D | Presence of nuclei and undersaturated water with respect to calcite. |
Question 31 |
A | at the asymmetric surfaces. |
B | at the trough of the dunes. |
C | at the points of flow convergence. |
D | at the peak of the crest (peak) of the dunes. |
E | along the troughs of parabolic bars. |
Question 32 |
A | Blue algae are adapted to deeper water environments and they absorbs red light. |
B | Green algae are adapted to shallow water environments and they absorbs yellow light. |
C | Green algae are adapted to deeper water environments and they absorbs red light. |
D | Red 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 | Red 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 | ...most abundant in shallow, protected environments. |
E | ...were exclusive to fresh water environments during Carboniferous and modern day they are exclusive to marine water environments. |
Question 34 |
A | Blue |
B | Red |
C | All types (Green, Blue and Red) |
D | Green |
Question 35 |
A | Some of them are capable of secreting or depositing carbonate around their body. |
B | They can be in several depositional settings such as marine, fresh-brackish water ponds, tidal flats and shallow sandy bottoms. |
C | They are important sediment produces and reef builders. |
D | This group includes both benthic and planktonic organisms that have the ability to photosynthesize. |
E | They are very important for economic resources such as diamond and gold ores. |
Question 36 |
A | Cynaophyta |
B | Rhodophyta |
C | Chlorophyta |
D | Chrysophyta |
Question 37 |
A | Yellow algae |
B | Blue algae |
C | Green algae |
D | Red algae |
Question 38 |
A | Tidal flats |
B | Open marines |
C | Restricted marine bays and lagoons |
D | Reef fronts |
E | Open marine bay shelf lagoons |
Question 39 |
A | I. cortex II. medulla |
B | I. central core II. outer core |
C | I. medulla II. cortex |
D | I. spinal core II. external core |
Question 40 |
A | Cretaceous |
B | Paleozoic |
C | Carboniferous |
D | Cenozoic |
E | Ediacaran |
Question 41 |
A | High energy water currents |
B | Sunlight and high energy water currents |
C | Sunlight and moisture |
D | Sunlight and availability of calcareous fluids |
E | Sunlight |
Question 42 |
A | Large portion of the mixing zone is in the marine diagenetic area. |
B | The best cementation processes occurs at shallow waters such as at the shelf or slopes. |
C | The partial pressure of CO2 is very high at shallow depths; leads to good cementation. |
D | CCD or carbon compensation depth is the depth in which the calcite start to become unstable. Hint: Nope; that would be Lysoclines |
E | Sediments could undergo marine diagenesis as long as water is present. |
Question 43 |
A | I. Blue II. green |
B | I. Red II. green |
C | I. Yellow II. green |
D | I. Green
II. red |
Question 44 |
A | alternating sediment-organic matter layers. |
B | lamination. |
C | layering. |
D | zoecias. |
E | pillars. |
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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