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Recognition of extraneous argon components through incremental-release analysis of biotite and hornblende across the Grenvillian metamorphic gradient in southwestern Labrador
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40Ar/39Ar muscovite ages from the Gagnon terrane of circa 970-910 Ma indicate that cooling to ~350°C in at least part of the terrane was rapid.
“40 Ar/ 39 Ar Ms ages from the Gagnon terrane of circa 970 -910 Ma [Dallmeyer and Rivers, 1983] indicate that cooling to $350°C in at least part of the terrane was rapid.”
From Grenville Front zone, Gagnon terrane, southwestern Labrador: Configuration of a midcrustal foreland fold‐thrust belt (2008) · cites this paper as Dallmeyer and Rivers, 1983
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Research works printed but not linked: 52
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Cited by
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van Gool, J. A. M., Rivers, T., & Calon, T. (2008) · Tectonics · doi:10.1029/2006tc002095 · Cited by 35
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Metadata
- Authors
- Dallmeyer, R. D., & Rivers, T.
- Venue
- Geochimica et Cosmochimica Acta
- Publisher
- Elsevier BV
- Published
- 1983-03
- Volume
- 47
- Issue
- 3
- Pages
- 413-428
- ISSN
- 0016-7037
- Cited by
- 53
- References
- 0
- Language
- en
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