| Reference Type | Journal (article/letter/editorial) |
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| Title | The Wyoming Province: a distinctive Archean craton in Laurentian North America |
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| Journal | Canadian Journal of Earth Sciences |
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| Authors | Mueller, P A | Author |
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| Frost, C D | Author |
| Year | 2006 (October 1) | Volume | 43 |
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| Page(s) | 1391-1397 | Issue | 10 |
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| Publisher | Canadian Science Publishing |
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| DOI | doi:10.1139/e06-075Search in ResearchGate |
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| Mindat Ref. ID | 484117 | Long-form Identifier | mindat:1:5:484117:7 |
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| GUID | ea1be48d-9a89-4d75-b9ae-ff0d68af6af3 |
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| Full Reference | Mueller, P A, Frost, C D (2006) The Wyoming Province: a distinctive Archean craton in Laurentian North America. Canadian Journal of Earth Sciences, 43 (10) 1391-1397 doi:10.1139/e06-075 |
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| Plain Text | Mueller, P A, Frost, C D (2006) The Wyoming Province: a distinctive Archean craton in Laurentian North America. Canadian Journal of Earth Sciences, 43 (10) 1391-1397 doi:10.1139/e06-075 |
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| In | (2006, October) Canadian Journal of Earth Sciences Vol. 43 (10) Canadian Science Publishing |
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| Abstract/Notes | The Wyoming Province is a distinctive Archean craton in the northwestern United States that can be subdivided into three subprovinces, namely, from oldest to youngest, the Montana metasedimentary province, the BeartoothâBighorn magmatic zone, and the Southern accreted terranes. Archean rocks of the Montana metasedimentary province and the BeartoothâBighorn magmatic zone are characterized by (1) their antiquity (rock ages to 3.5 Ga, detrital zircon ages up to 4.0 Ga, and Nd model ages exceeding 4.0 Ga); (2) a distinctly enriched 207Pb/204Pb isotopic signature, which suggests that this part of the province was not produced by the amalgamation of exotic terranes; and (3) a distinctively thick (15â20 km), mafic lower crust. The Montana metasedimentary province and BeartoothâBighorn magmatic zone were cratonized by about 3.0â2.8 Ga. Crustal growth occurred via continental-arc magmatism and terrane accretion in the Southern accreted terranes along the southern margin of the province at 2.68â2.50 Ga. By the end of the Archean, the three subprovinces were joined as part of what is now the Wyoming Province. Subsequent to amalgamation of the Wyoming crust to Laurentia at ca. 1.8â1.9 Ga, Paleoproterozoic crust (1.7â2.4 Ga) was juxtaposed along the southern and western boundaries of the province. Subsequent tectonism and magmatism in the Wyoming region are concentrated in the areas underlain by these Proterozoic mobile belts. |
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These are the references the publisher has listed as being connected to the article. Please check the article itself for the full list of references which may differ. Not all references are currently linkable within the Digital Library.
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