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Rodinia, Rifting, Iapetus and the Great American Bank
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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
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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
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The Grenville Province
Last Precambrian Orogeny in North America Ga Regional metamorphism from Maritime Canada to Georgia Last event in the assembly of the supercontinent Rodinia
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Grenville Gneiss
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Assembling Rodinia: the Grenville Orogeny
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Rodinia – a supercontinent 700 Ma before Pangea
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Potsdam (C) – Grenville (Pre-C) Nonconformity in New York
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Precambrian – Cambrian Nonconformity - Colorado
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Precambrian – Cambrian Nonconformity – Grand Canyon, AZ
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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
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Rifting Rodinia – Opening the Iapetus Ocean, Birth of the Great American Bank
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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
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Wading in Iapetus - Stromatolites
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Wading in Iapetus – Quartz Arenites, Limestones, Burrows & Ripples
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Great American Bank Carbonates – Mohawk Valley, New York
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