Neodymium isotopic evidence for the tectonic assembly of Late Archean crust in the Slave Province, northwest Canada

Contributions to Mineralogy and Petrology

Volumn 111, Issue 4, 1992, Pages 493-504

  Davis, William J ^a   Hegner, Ernst ^b  

^a MEMORIAL UNIVERSITY OF NEWFOUNDLAND   (Canada)

^b GEOLOGICAL SURVEY OF CANADA   (Canada)

Author keywords

[No Author keywords available]

Indexed keywords

EID: 30744466309     PISSN: 00107999     EISSN: 14320967     Source Type: Journal    
DOI: 10.1007/BF00320904     Document Type: Article

References (89)

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16. Structural patterns and tectonic evolution of supracrustal domains in the Archean Slave Province, Canada
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18. A Sm-Nd isotopic study of atmospheric dust and particulates from major river systems
19. A new look at the stratigraphy of the Yellowknife Supergroup at Yellowknife, NWT — implications for the age of gold-bearing shear zones and Archean basin evolution
20. Archean basin evolution in the Slave Province, Canada
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29. U-Pb isotopic ages of basement and supracrustal rocks in the Point Lake area of the Slave Structural Province, Canada (abstract)
30. Accretion of the Archean Slave Province
31. Evidence for Archean ocean opening and closing in the southern Slave Province
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36. Archean custal evolution — a glimpse from the Slave Province
37. Geochemistry of Cenozoic volcanic rocks, Baja California, Mexico: implications for the petrogensis of post-subduction magmas
38. Investigations of the Archean crust by single grain dating of detrital zircon: a greywacke of the Slave Province, Canada
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43. Implications for the evolution of continental crust from Hf isotope systematics of Archean detrital zirons
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48. Interpretation of lead isotope data for base metal and gold deposits, Slave Province
49. Nd, O and Sr isotopic constraints on the origin of Precambrian rocks, Southern Black Hills, South Dakota
50. New tectonic models for the evolution of Archean continents and oceans
51. Pb, Sr and Nd isotopic compositions of a suite of Late Archean igneous rocks, eastern Beartooth Mountains: implications for crust-mantle evolution