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