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“However, the time-related decrease in the LREE/HREE ratios coupled with higher contents of compatible elements (e.g., MgO, Sc) cannot be modeled as a simple fractional crystallization process from a basaltic magma with Réunion-like compositions combined with assimilation of typical upper or lower crustal compositions (e.g., Rudnick & Gao, 2003).”
From Geochronological Constraints on the Evolution and Petrogenesis of the Malwa Plateau Subprovince of the Deccan Traps (2023) · cites this paper as Rudnick & Gao, 2003
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The geochemical evolution of the continental crust
Taylor, S. R., & McLennan, S. M. (1995) · Reviews of Geophysics · doi:10.1029/95rg00262 · Cited by 4,643
Nature and composition of the continental crust: A lower crustal perspective
Rudnick, R. L., & Fountain, D. M. (1995) · Reviews of Geophysics · doi:10.1029/95rg01302 · Cited by 3,323
Self-citationSeismic velocity structure and composition of the continental crust: A global view
Christensen, N. I., & Mooney, W. D. (1995) · Journal of Geophysical Research: Solid Earth · doi:10.1029/95jb00259 · Cited by 2,952
Wilde, S. A., Valley, J. W., Peck, W. H., & Graham, C. M. (2001) · Nature · doi:10.1038/35051550 · Cited by 1,744
Priscoan (4.00–4.03 Ga) orthogneisses from northwestern Canada
Bowring, S. A., & Williams, I. S. (1999) · Contributions to Mineralogy and Petrology · doi:10.1007/s004100050465 · Cited by 568 · cited 1×
“…(Taylor and McLennan (1985) and references therein), and contains the oldest rocks and minerals yet observed on Earth (currently the 4.0 Ga Acasta gneisses (Bowring and Williams, 1999) and 4.4 Ga detrital zircons from the Yilgarn Block, Western Australia (Wilde et al., 2001)), respectively.”
InfluentialThe global resurfacing of Venus
Strom, R. G., Schaber, G. G., & Dawson, D. D. (1994) · Journal of Geophysical Research: Planets · doi:10.1029/94je00388 · Cited by 400
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Metadata
- Authors
- Rudnick, R. L., & Gao, S.
- Venue
- Treatise on Geochemistry
- Publisher
- Elsevier
- Published
- 2003
- Pages
- 1-64
- Cited by
- 3,413
- References
- 6
- Language
- en
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