Biblio
Recovering compressively sampled signals using partial support information. IEEE Transactions on Information Theory. 58:1122-1134.
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2012. Discussion: the Dantzig selector: statistical estimation when p is much larger than n. The Annals of Statistics. 35:2385-2391.
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2007. Exact regularization of convex programs. SIAM Journal on Optimization. 18:1326-1350.
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2007. Hybrid deterministic-stochastic methods for data fitting. SIAM Journal on Scientific Computing. 34:A1380-A1405.
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2012. Origin and evolution of a submarine large igneous province: the Kerguelen Plateau and Broken Ridge, southern Indian Ocean. Earth and Planetary Science Letters. 176:73–89.
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2000. Reply to the Class et al. discussion of “Temporal evolution of the Kerguelen plume: geochemical evidence from 38 to 82 Ma lavas forming the Ninetyeast Ridge”. Contributions to Mineralogy and Petrology. 124:104–110.
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1996. Components of Continental Crust in the Kerguelen Plateau and Broken Ridge-Involvement of Continental Crust in the Formation of the Cretaceous Kerguelen Plateau: New Perspectives from ODP Leg 120. Journal of Petrology. 43:1207–1240.
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2002. Involvement of continental crust in the formation of the Cretaceous Kerguelen Plateau: new perspectives from ODP Leg 120 sites. Journal of Petrology. 43:1207–1239.
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2002. Temporal evolution of the Kerguelen plume: geochemical evidence from 38 to 82 Ma lavas forming the Ninetyeast Ridge. Oceanographic Literature Review. 10:1013.
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1996. Leg 183 synthesis: Kerguelen Plateau-Broken Ridge—a large igneous province. Proc. Ocean Drill. Program Sci. Results. 183:1–48.
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2003. Temporal evolution of the Kerguelen plume: Geochemical evidence from 38 to 82 Ma lavas forming the Ninetyeast Ridge. Contributions to Mineralogy and Petrology. 121:12–28.
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1995. CD-ROM: ISSN 1096-2514. www-odp.tamu.edu.
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Submitted. Kerguelen plume: A 120 Myr record of volcanism. Geochimica et Cosmochimica Acta Supplement. 67:104.
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2003. Temporal evolution of the Kerguelen plume: Geochemical evidence from 38 to 82 Ma lavas forming the Ninetyeast Ridge. Contributions to Mineralogy and Petrology.
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1995. .
Submitted. Involvement of continental crust in the formation of the Cretaceous Kerguelen Plateau: new perspectives from ODP Leg 120 sites. Journal of Petrology.
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2002. Depleted components in the source of hotspot magmas: Evidence from the Ninetyeast Ridge (Kerguelen). Earth and Planetary Science Letters. 426:293–304.
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2015. Flood basalt from Mont Tourmente in the Central Kerguelen Archipelago: the change from transitional to alkalic basalt at∼ 25 Ma. Journal of ….
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2002. Flood basalt from Mont Tourmente in the Central Kerguelen Archipelago: the change from transitional to alkalic basalt at 25 Ma. Journal of Petrology. 43:1367–1387.
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2002. Depleted components in the source of hotspot magmas: Evidence from the Ninetyeast Ridge (Kerguelen). Earth and Planetary ….
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2015. Temporal geochemical trends in Kerguelen Archipelago basalts: evidence for decreasing magma supply from the Kerguelen plume. Chemical Geology. 164:61–80.
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2000. Millard F. Coffin Co-Chief Scientist. Ann Arbor MI.
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Submitted. Reply to the Class et al. discussion of" Temporal evolution of the Kerguelen plume: geochemical evidence from asymptotically equal to 38 to 82 Ma lavas forming the Ninetyeast Rige". CONTRIBUTIONS TO MINERALOGY AND PETROLOGY. 124:104–110.
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1996. .
2002. What have we learned:\~ 120 myr of Kerguelen Plume activity? EGS-AGU-EUG Joint Assembly.
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2003.