Rodinia, Rifting, Iapetus and the Great American Bank - PowerPoint PPT Presentation

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Rodinia, Rifting, Iapetus and the Great American Bank

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Cratons parts of shield with thin cover of sedimentary rocks ... more inboard position less subsidence. Wading in Iapetus - Stromatolites. Wading in Iapetus ... – PowerPoint PPT presentation

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Title: Rodinia, Rifting, Iapetus and the Great American Bank


1
Rodinia, Rifting, Iapetus and the Great American
Bank
2
General Structure of Continents
  • Shields old, tectonically stable foundation of
    continent
  • Cratons parts of shield with thin cover of
    sedimentary rocks
  • Passive Margins continental shelves, mid-plate
  • Convergent Margins zones of subduction and
    collision at edge of plate

3
Precambrian Shield
  • Predominantly crystalline (granite gneiss)
  • Divided into Provinces by age and structureal
    grain
  • Provinces represent the roots of long gone
    mountains
  • Each Province produced during a specific Orogeny
  • Narrow greenstone belts
  • Commonly between provinces
  • Metamorphosed mafic volcanics
  • Ophiolites
  • Immature sedimentary rocks
  • Remnants of subducted oceanic lithosphere

4
The Grenville Province
  • Last Precambrian Orogeny in North America
  • 1.2-0.9 Ga
  • Regional metamorphism from Maritime Canada to
    Georgia
  • Last event in the assembly of the supercontinent
    Rodinia

5
Grenville Gneiss
6
Assembling Rodiniathe Grenville Orogeny
7
Rodinia a supercontinent 700 Ma before Pangea
8
Potsdam (C) Grenville (Pre-C) Nonconformity in
New York
9
Precambrian Cambrian Nonconformity - Colorado
10
Precambrian Cambrian Nonconformity Grand
Canyon, AZ
11
Precambrian Cambrian Nonconformity
  • Widespread across North America
  • Extensive erosion of shield and Grenville Orogen
    (Mountains)
  • Worldwide Transgression in Latest Precambrian
    into Cambrian
  • Similar pattern on other continents
  • Post-unconformity rocks are Quartz Arenites and
    Limestones
  • Typical cratonic association

12
Rifting Rodinia Opening the Iapetus Ocean,
Birth of the Great American Bank
13
Great American Bank
  • Opening of Iapetus Ocean
  • Creates passive margin
  • Thermal subsidence produces accommodation space
  • Thousands of meters of quartz arenites and
    limestones/dolomites deposited in shallow water
  • Stromatolites, Mudcracks, Intraclasts
  • Exposed in Cumberland/Great Valley and Shenandoah
    Valley
  • Sequence is thinner in New York
  • more inboard position less subsidence

14
Wading in Iapetus - Stromatolites
15
Wading in Iapetus Quartz Arenites,
Limestones,Burrows Ripples
16
Great American Bank Carbonates Mohawk Valley,
New York
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