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- W2498288524 abstract "Research on the Precambrian basement of North America over the past two decades has shown that Archean and earliest Proterozoic evolution culminated in suturing of Archean cratonic elements and pre-1.80-Ga Proterozoic terranes to form the Canadian Shield at about 1.80 Ga (Hoffman, 1988,1989a, b). We will refer to this part of Laurentia as the Hudsonian craton (Fig. 1) because it was fused together about 1.80 to 1.85 Ga during the Trans-Hudson and Penokean orogenies (Hoffman, 1988). The Hudsonian craton, including its extensions into the United States (Chapters 2 and 3, this volume), formed the foreland against which 1.8- to 1.6-Ga continental growth occurred, forming the larger Laurentia (Hoffman, 1989a, b). Geologic and geochronologic studies over the past three decades have shown that most of the Precambrian in the United States south of the Hudsonian craton and west of the Grenville province (Chapter 5) consists of a broad northeast to east-northeast-trending zone of orogenic provinces that formed between 1.8 and 1.6 Ga. This zone, including extensions into eastern Canada, comprises or hosts most rock units of this age in North America as well as extensive suites of 1.35- to 1.50-Ga granite and rhyolite. This addition to the Hudsonian Craton is referred to in this chapter as the Transcontinental Proterozoic provinces (Fig. 1); the plural form is used to denote the composite nature of this broad region. The Transcontinental Proterozoic provinces consist of many distinct lithotectonic entities that can be defined on the basis of regional lithology, regional structure, U-Pb ages from zircons, Sr-Nd-Pb isotopic signatures, and regional geophysical anomalies." @default.
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- W2498288524 date "2015-04-05" @default.
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- W2498288524 title "Transcontinental Proterozoic provinces" @default.
- W2498288524 cites W117063972 @default.
- W2498288524 cites W119482154 @default.
- W2498288524 cites W1242895745 @default.
- W2498288524 cites W1424996432 @default.
- W2498288524 cites W1510585873 @default.
- W2498288524 cites W1579495885 @default.
- W2498288524 cites W1582572988 @default.
- W2498288524 cites W1598335788 @default.
- W2498288524 cites W1607810287 @default.
- W2498288524 cites W1608960209 @default.
- W2498288524 cites W1666465879 @default.
- W2498288524 cites W1856932658 @default.
- W2498288524 cites W1886688909 @default.
- W2498288524 cites W188968803 @default.
- W2498288524 cites W1965000870 @default.
- W2498288524 cites W1966212987 @default.
- W2498288524 cites W1967021081 @default.
- W2498288524 cites W1968002297 @default.
- W2498288524 cites W1969065246 @default.
- W2498288524 cites W1969599847 @default.
- W2498288524 cites W1971706508 @default.
- W2498288524 cites W1972669556 @default.
- W2498288524 cites W1974881922 @default.
- W2498288524 cites W1977650828 @default.
- W2498288524 cites W1978575527 @default.
- W2498288524 cites W1979331501 @default.
- W2498288524 cites W1979350315 @default.
- W2498288524 cites W1979694457 @default.
- W2498288524 cites W1979884913 @default.
- W2498288524 cites W1980443113 @default.
- W2498288524 cites W1981117492 @default.
- W2498288524 cites W1983596468 @default.
- W2498288524 cites W1984744184 @default.
- W2498288524 cites W1986306461 @default.
- W2498288524 cites W1989577524 @default.
- W2498288524 cites W1989986197 @default.
- W2498288524 cites W1990624497 @default.
- W2498288524 cites W1990674890 @default.
- W2498288524 cites W1993804022 @default.
- W2498288524 cites W1994928384 @default.
- W2498288524 cites W1995690166 @default.
- W2498288524 cites W1995753299 @default.
- W2498288524 cites W1996322558 @default.
- W2498288524 cites W1998788737 @default.
- W2498288524 cites W1999033332 @default.
- W2498288524 cites W1999602453 @default.
- W2498288524 cites W2000229631 @default.
- W2498288524 cites W2000787898 @default.
- W2498288524 cites W2001269981 @default.
- W2498288524 cites W2002004285 @default.
- W2498288524 cites W2003666178 @default.
- W2498288524 cites W2003694462 @default.
- W2498288524 cites W2003761134 @default.
- W2498288524 cites W2004042049 @default.
- W2498288524 cites W2004401211 @default.
- W2498288524 cites W2004775384 @default.
- W2498288524 cites W2005923562 @default.
- W2498288524 cites W2006493918 @default.
- W2498288524 cites W2006987475 @default.
- W2498288524 cites W2007105153 @default.
- W2498288524 cites W2007417704 @default.
- W2498288524 cites W2009004065 @default.
- W2498288524 cites W2009292745 @default.
- W2498288524 cites W2009395575 @default.
- W2498288524 cites W2009485390 @default.
- W2498288524 cites W2010533300 @default.
- W2498288524 cites W2011353760 @default.
- W2498288524 cites W2011745116 @default.
- W2498288524 cites W2011815411 @default.
- W2498288524 cites W2012913935 @default.