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Metamorphism

Izzy Backhouse 7 questions

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  1. 1Metamorphism = the [blank_start]isochemical[blank_end] process by which rocks are changed through [blank_start]solid-state[blank_end] [blank_start]recrystallisation[blank_end] by temperature and/or [blank_start]pressure[blank_end] into a new rock with the same [blank_start]chemical composition[blank_end] as the [blank_start]parent[blank_end]
    1. Aisochemical
    2. Bsolid-state
    3. Crecrystallisation
    4. Dpressure
    5. Echemical composition
    6. Fparent
  2. 2The lower temperature limit of metamorphism is [blank_start]200[blank_end] oC.
    The upper temperature limit of metamorphism is [blank_start]800[blank_end] oC.
    1. A200
    2. B150
    3. C100
    4. D750
    5. E800
    6. F900
  3. 3[blank_start]Isochemical[blank_end] = No elements are added or removed except for volatiles eg. carbon dioxide and water.
    1. AIsochemical
  4. 4Metamorphism may result in:
    - Destruction of [blank_start]fossils[blank_end], beds and [blank_start]sedimentary structures[blank_end]
    - Growth of new [blank_start]metamorphic minerals[blank_end]
    - [blank_start]Alignment[blank_end] of minerals
    - [blank_start]Hardening[blank_end] of rock
    - Change in [blank_start]colour[blank_end]
    1. Afossils
    2. Bsedimentary structures
    3. Cmetamorphic minerals
    4. DAlignment
    5. EHardening
    6. Fcolour
  5. 5- Temperature increases with [blank_start]depth[blank_end] due to the [blank_start]geothermal gradient[blank_end].
    - High temperatures occur near to [blank_start]igneous intrusions[blank_end] as the magma there heats the surrounding rocks.
    - As temperature increases, the [blank_start]rate[blank_end] of metamorphic reactions increases because many chemical reactions require [blank_start]heat[blank_end] to take place.
    - [blank_start]Higher[blank_end] temperatures increases the rate at which ions [blank_start]diffuse[blank_end] between minerals.
    - Metamorphism can be sped up by [blank_start]water[blank_end] which allows the [blank_start]ions[blank_end] to be diffused more rapidly.
    1. Adepth
    2. Bgeothermal gradient
    3. Cigneous intrusions
    4. Drate
    5. Eheat
    6. FHigher
    7. Gdiffuse
    8. Hwater
    9. Iions
  6. 6[blank_start]Load pressure[blank_end] = the weight of [blank_start]overlying[blank_end] rocks that physically brings minerals into contact into each other over very long periods of time.
    [blank_start]Pore pressure[blank_end] = pressure exerted by [blank_start]fluids[blank_end] between the grains in a porous rocks.
    [blank_start]Tectonic pressure[blank_end] = caused as the rocks undergo faulting or folding, exerting high pressures over relatively [blank_start]short[blank_end] periods of time.
    1. ALoad pressure
    2. BPore pressure
    3. CTectonic Pressure
    4. DPore pressure
    5. ELoad pressure
    6. FTectonic pressure
    7. GTectonic pressure
    8. HLoad pressure
    9. IPore pressure
    10. Junderlying
    11. Koverlying
    12. Ladjacent
    13. Mfluids
    14. Nsolids
    15. Ogases
    16. Pshort
    17. Qlong
  7. 7Describe regional metamorphism produced at low grade.
    - Low grade metamorphic rock: [blank_start]slate[blank_end]
    - Temperatures and pressures: [blank_start]low[blank_end]
    - Crystal grain size: [blank_start]fine[blank_end]
    - Index mineral: [blank_start]chlorite[blank_end]
    - muscovite formed by: [blank_start]recrystallisation[blank_end]
    - formation of [blank_start]slaty cleavage[blank_end] (texture) with minerals aligned at [blank_start]90[blank_end] degrees to pressure.
    - Porphyroblasts of [blank_start]pyrite[blank_end] may form
    Image for question 7
    1. Aslate
    2. Blow
    3. Cfine
    4. Dchlorite
    5. Erecrystallisation
    6. Fslaty cleavage
    7. G90
    8. Hpyrite

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Description
AS - Level Geology (F792) Quiz on Metamorphism, created by Izzy Backhouse on 17/04/2016.
Language
English
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