Biblio
Supraglacial channel inception: Modeling and processes. WATER RESOURCES RESEARCH. 51:7044-7063.
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2015. Surface formation, preservation, and history of low-porosity crusts at the WAIS Divide site, West Antarctica. The Cryosphere. 12:325.
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2018. Surface formation, preservation, and history of low-porosity crusts at the WAIS Divide site, West Antarctica. The Cryosphere. 12:325.
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2018. Surface studies of water isotopes in Antarctica for quantitative interpretation of deep ice core data. Comptes Rendus Geoscience. 349:139–150.
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2017. Surface studies of water isotopes in Antarctica for quantitative interpretation of deep ice core data. Comptes Rendus Geoscience. 349:139–150.
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2017. Surface temperature in twentieth century at the Styx Glacier, northern Victoria Land, Antarctica, from borehole thermometry. Geophysical Research Letters. 45:9834–9842.
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2018. Surface temperature in twentieth century at the Styx Glacier, northern Victoria Land, Antarctica, from borehole thermometry. Geophysical Research Letters. 45:9834–9842.
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2018. Surface tension driven processes densify and retain permeability in magma and lava. EARTH AND PLANETARY SCIENCE LETTERS. 433:116-124.
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2016. Suspended particles in the Canada Basin from optical and bottle data, 2003-2008. OCEAN SCIENCE. 6:799-813.
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2010. .
Submitted. Tadhak alkaline ring-complex (Mali): existence of U Pb isochrons and “Dupal” signature 270 Ma ago. Earth and planetary science letters. 82:316–322.
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1987. Tails of two plume types in one mantle. GEOLOGY. 37:127-130.
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2009. Tectónica y geoqu{ímica de la Formación Amina: registro del arco isla Caribeño primitivo en la Cordillera Central, República Dominicana. Bolet{ín geológico y minero. 118:221–242.
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2007. Tectono-stratigraphic setting of the Moreton’s Harbour Group and its implications for the evolution of the Laurentian margin: Notre Dame Bay, Newfoundland. Canadian Journal of Earth Sciences. 49:111-127.
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2012. 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. 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. 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. 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.
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1996. 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. Temporal geochemical variations in lavas from K\=ılauea's Pu ‘u ‘\=O ‘ō eruption (1983–2010): Cyclic variations from melting of source heterogeneities. Geochemistry, Geophysics, Geosystems. 14:4849–4873.
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2013. Temporal geochemical variations in lavas from Kīlauea's Pu 'u 'Ō 'ō eruption (1983–2010): Cyclic variations from melting of source heterogeneities. Geochemistry, ….
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2013. Temporal isotopic variations in the Kerguelen plume: evidence from the Kerguelen Archipelago. Miner. Mag. A. 62:1643–1644.
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1998. TEXTURAL ANALYSIS OF STRONGLY ALTERED KIMBERLITE: EXAMPLES FROM THE EKATI DIAMOND MINE, NORTHWEST TERRITORIES, CANADA. The Canadian Mineralogist. 50:625–641.
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2012. TEXTURAL ANALYSIS OF STRONGLY ALTERED KIMBERLITE: EXAMPLES FROM THE EKATI DIAMOND MINE, NORTHWEST TERRITORIES, CANADA. CANADIAN MINERALOGIST. 50:625-641.
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2012. Tharsis as a consequence of Mars' dichotomy and layered mantle. GEOPHYSICAL RESEARCH LETTERS. 31
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2004.