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TitleThe tectonic evolution of Laurentia and the North American continent: new datasets, insights, and models
 
AuthorWhitmeyer, S J; Kellett, D AORCID logo; Tikoff, B; Williams, M L
SourceLaurentia: turning points in the evolution of a continent; Geological Society of America, Memoir vol. 220, 2023 p. 7-16, https://doi.org/10.1130/2022.1220(001)
Image
Year2023
Alt SeriesNatural Resources Canada, Contribution Series 20210545
PublisherGeological Society of America
Documentserial
Lang.English
Map Info.location, 1:44,000,000
Mediapaper; digital; on-line
File formatpdf; html
NTS1; 2; 3; 10; 11; 12; 13; 14; 15; 16; 20; 21; 22; 23; 24; 25; 26; 27; 28; 29; 30; 31; 32; 33; 34; 35; 36; 37; 38; 39; 40; 41; 42; 43; 44; 45; 46; 47; 48; 49; 52; 53; 54; 55; 56; 57; 58; 59; 62; 63; 64; 65; 66; 67; 68; 69; 72; 73; 74; 75; 76; 77; 78; 79; 82; 83; 84; 85; 86; 87; 88; 89; 92; 93; 94; 95; 96; 97; 98; 99; 102; 103; 104; 105; 106; 107; 114O; 114P; 115; 116; 117; 120; 340; 560
AreaNorth America
Lat/Long WENS-141.0000 -50.0000 90.0000 41.7500
Lat/Long WENS 0.0000 0.0000 -2000.0000 -2000.0000
SubjectsScience and Technology; tectonics; Nature and Environment; rivers; lakes; physiography; Laurentia; Boundaries
Illustrationsgraphs
ProgramGEM2: Geo-mapping for Energy and Minerals GEM Synthesis
Released2023 01 09
AbstractThe North American continent has a rich geologic record that preserves evidence for tectonic processes throughout much of Earth's history. Within this long history, however, particular times-e.g., "turning points"—have had specific and lasting impact on the evolution of Laurentia (ancestral North America). This volume is focused on seven of these "turning points": (1) The Neoarchean (2.7-2.5 Ga), characterized by cratonization and the Kenoran orogen(s); (2) the Paleoproterozoic (1.9-1.7 Ga) and the initial assembly of Laurentia; (3) the Mesoproterozoic (1.5-1.4 Ga) Andean-style margin on the southern edge of Laurentia with the Pinware-Baraboo-Picuris orogeny; (4) the 1.2-1.0 Ga Midcontinent rift, and the Grenville orogeny and assembly of Rodinia; (5) the 700-500 Ma Neoproterozoic breakup of Rodinia; (6) the mid-Paleozoic (420-340 Ma) closure of the Iapetus and Rheic oceans and the development of the Appalachian-Caledonian orogen; and (7) the Jurassic-Paleogene (200-50 Ma) assembly of the North American Cordilleran margin by terrane accretion and subduction. The assembled chapters provide syntheses of current understanding of the geologic evolution of Laurentia and North America, as well as new hypotheses for testing. The inclusion of work from different geological time periods within a single volume provides continent-wide perspectives on the evolution of tectonic events and processes that acted on and within Laurentia.
Summary(Plain Language Summary, not published)
This is the introductory chapter to a Geological Society of America Memoir on the geological evolution of Laurentia. Chapter contributions are based upon a Pardee symposium and seven related special sessions held at the virtual 2020 Geological Society of America annual meeting. Contributions cover new data, insights and models for seven critical time periods in Laurentia's geological history.
GEOSCAN ID329439

 
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