Publications
Identifying biological landmarks using a novel cell measuring image analysis tool: Cell-o-Tape. PLANT METHODS. 8
. 2012. Millard F. Coffin Co-Chief Scientist. Ann Arbor MI.
. Submitted. 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.
. 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.
. 1996. 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.
. 2002. Kerguelen Plateau-Broken Ridge: a large igneous province. Proc. ODP Init. Rep. 183
. Submitted. Leg 183 synthesis: Kerguelen Plateau-Broken Ridge—a large igneous province. Proc. Ocean Drill. Program Sci. Results. 183:1–48.
. 2003. . 2002. Millard F. Coffin Co-Chief Scientist. Ann Arbor MI. 48109:1063.
. Submitted. 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.
. 1995. Temporal evolution of the Kerguelen plume: Geochemical evidence from 38 to 82 Ma lavas forming the Ninetyeast Ridge. Contributions to Mineralogy and Petrology.
. 1995. 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.
. 2002. Temporal evolution of the Kerguelen plume: geochemical evidence from 38 to 82 Ma lavas forming the Ninetyeast Ridge. Oceanographic Literature Review. 10:1013.
. 1996. Flood basalt from Mont Tourmente in the Central Kerguelen Archipelago: the change from transitional to alkalic basalt at∼ 25 Ma. Journal of ….
. 2002. 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.
. 1996. Involvement of continental crust in the formation of the Cretaceous Kerguelen Plateau: new perspectives from ODP Leg 120 sites. Journal of Petrology.
. 2002. . Submitted. Depleted components in the source of hotspot magmas: Evidence from the Ninetyeast Ridge (Kerguelen). Earth and Planetary ….
. 2015. CD-ROM: ISSN 1096-2514. www-odp.tamu.edu.
. Submitted. . Submitted. Northern Kerguelen Plateau and Kerguelen Archipelago: Mantle Sources and Magmatic Processes-Flood Basalt from Mont Tourmente in the Central Kerguelen Archipelago: The Change from Transitional to. Journal of Petrology. 43:1367–1388.
. 2002. Depleted components in the source of hotspot magmas: Evidence from the Ninetyeast Ridge (Kerguelen). Earth and Planetary Science Letters. 426:293–304.
. 2015. 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.
. 2002. Temporal geochemical trends in Kerguelen Archipelago basalts: evidence for decreasing magma supply from the Kerguelen plume. Chemical Geology. 164:61–80.
. 2000. Temporal evolution of the Kerguelen plume: Geochemical evidence from approximate to 38 to 82 Ma lavas forming the Ninetyeast ridge-Reply. CONTRIBUTIONS TO MINERALOGY AND PETROLOGY. 124:104–110.
. 1996.