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Rodinia, Rifting, Iapetus and the Great American Bank

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Presentation on theme: "Rodinia, Rifting, Iapetus and the Great American Bank"— Presentation transcript:

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 Ga Regional metamorphism from Maritime Canada to Georgia Last event in the assembly of the supercontinent Rodinia

5 Grenville Gneiss

6 Assembling Rodinia: the 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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