Search Results - "V. Debaille"

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    The evolution of Hadean–Eoarchaean geodynamics by O'Neill, C., Debaille, V.

    Published in Earth and planetary science letters (01-11-2014)
    “…Geodynamic modelling of Hadean/Eoarchaean tectonics typically requires higher rates of internal heat production, and higher mantle temperatures, in models that…”
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    Dry late accretion inferred from Venus’s coupled atmosphere and internal evolution by Gillmann, C., Golabek, G. J., Raymond, S. N., Schönbächler, M., Tackley, P. J., Dehant, V., Debaille, V.

    Published in Nature geoscience (01-04-2020)
    “…It remains contentious whether the meteoritic material delivered to the terrestrial planets after the end of core formation was rich or poor in water and other…”
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    Long-Term Evolution of the Martian Crust-Mantle System by Grott, M., Baratoux, D., Hauber, E., Sautter, V., Mustard, J., Gasnault, O., Ruff, S. W., Karato, S.-I., Debaille, V., Knapmeyer, M., Sohl, F., Van Hoolst, T., Breuer, D., Morschhauser, A., Toplis, M. J.

    Published in Space science reviews (01-01-2013)
    “…Lacking plate tectonics and crustal recycling, the long-term evolution of the crust-mantle system of Mars is driven by mantle convection, partial melting, and…”
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    Younger Age for ALH84001 and Its Geochemical Link to Shergottite Sources in Mars by Lapen, T.J, Righter, M, Brandon, A.D, Debaille, V, Beard, B.L, Shafer, J.T, Peslier, A.H

    “…Martian meteorite ALH84001 (ALH) is the oldest known igneous rock from Mars and has been used to constrain its early history. Lutetium-hafnium (Lu-Hf) isotope…”
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    Structural and Geochemical Interactions Between Magma and Sedimentary Host Rock: The Hovedøya Case, Oslo Rift, Norway by S. Poppe, O. Galland, N. J. deWinter, S. Goderis, P. Claeys, V. Debaille, P. Boulvais, M. Kervyn

    Published in Geochemistry, geophysics, geosystems : G3 (01-03-2020)
    “…Abstract Two end‐member conceptual models are used to describe deformation of the Earth's crust induced by magma intrusion. “Mode I” fracturing assumes tensile…”
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    Obsidian and mafic volcanic glasses from the Philippines and Vietnam found in the Paris Museum Australasian tektite collection by Rochette, P., Bezaeva, N. S., Beck, P., Debaille, V., Folco, L., Gattacceca, J., Gounelle, M., Masotta, M.

    Published in Meteoritics & planetary science (01-07-2022)
    “…During the systematic magnetic susceptibility survey of the Paris Museum Australasian tektite collection, we identified three previously overlooked occurrences…”
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    Early martian mantle overturn inferred from isotopic composition of nakhlite meteorites by Debaille, V, Yin, Q.-Z, Jacobsen, B, O'Neill, C, Brandon, A. D

    Published in Nature geoscience (01-08-2009)
    “…The early stages of planetary differentiation are characterized by the formation of magma oceans, which crystallize from the base up. The final, iron-rich…”
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    Differentiation and magmatic activity in Vesta evidenced by 26Al-26Mg dating in eucrites and diogenites by Hublet, G., Debaille, V., Wimpenny, J., Yin, Q-Z.

    Published in Geochimica et cosmochimica acta (01-12-2017)
    “…The 26Al-26Mg short-lived chronometer has been widely used for dating ancient objects in studying the early Solar System. Here, we use this chronometer to…”
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    Impact mixing among rocky planetesimals in the early Solar System from angrite oxygen isotopes by Rider-Stokes, B. G., Greenwood, R. C., Anand, M., White, L. F., Franchi, I. A., Debaille, V., Goderis, S., Pittarello, L., Yamaguchi, A., Mikouchi, T., Claeys, P.

    Published in Nature astronomy (01-07-2023)
    “…Angrite meteorites are thought to represent ancient basaltic igneous rocks that formed inward of Jupiter’s orbit on the basis of their isotopic parameters such…”
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    Caleta el Cobre 022 Martian meteorite: Increasing nakhlite diversity by Krämer Ruggiu, L., Gattacceca, J., Devouard, B., Udry, A., Debaille, V., Rochette, P., Lorand, J.‐P., Bonal, L., Beck, P., Sautter, V., Busemann, H., Meier, M. M. M., Maden, C., Hublet, G., Martinez, R.

    Published in Meteoritics & planetary science (01-07-2020)
    “…Caleta el Cobre (CeC) 022 is a Martian meteorite of the nakhlite group, showing an unbrecciated cumulate texture, composed mainly of clinopyroxene and olivine…”
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    Pantasma: Evidence for a Pleistocene circa 14 km diameter impact crater in Nicaragua by Rochette, P., Alaç, R., Beck, P., Brocard, G., Cavosie, A. J., Debaille, V., Devouard, B., Jourdan, F., Mougel, B., Moustard, F., Moynier, F., Nomade, S., Osinski, G. R., Reynard, B., Cornec, J.

    Published in Meteoritics & planetary science (01-04-2019)
    “…The circa 14 km diameter Pantasma circular structure in Oligocene volcanic rocks in Nicaragua is here studied for the first time to understand its origin…”
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    The case for metamorphic base metal mineralization: pyrite chemical, Cu and S isotope data from the Cu-Zn deposit at Kupferberg in Bavaria, Germany by Höhn, S., Frimmel, H.E., Debaille, V., Pašava, J., Kuulmann, L., Debouge, W.

    Published in Mineralium deposita (01-12-2017)
    “…The stratiform Cu-Zn sulfide deposit at Kupferberg in Germany represents Bavaria’s largest historic base metal producer. The deposit is hosted by Early…”
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    The formation of IIE iron meteorites investigated by the chondrule-bearing Mont Dieu meteorite by Van Roosbroek, N., Debaille, V., Pittarello, L., Goderis, S., Humayun, M., Hecht, L., Jourdan, F., Spicuzza, M. J., Vanhaecke, F., Claeys, Ph

    Published in Meteoritics & planetary science (01-07-2015)
    “…A 435 kg piece of the Mont Dieu iron meteorite (MD) contains cm‐sized silicate inclusions. Based on the concentration of Ni, Ga, Ge, and Ir (8.59 ± 0.32 wt%,…”
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    A large meteoritic event over Antarctica ca. 430 ka ago inferred from chondritic spherules from the Sør Rondane Mountains by Van Ginneken, M, Goderis, S, Artemieva, N, Debaille, V, Decrée, S, Harvey, R P, Huwig, K A, Hecht, L, Yang, S, Kaufmann, F E D, Soens, B, Humayun, M, Van Maldeghem, F, Genge, M J, Claeys, P

    Published in Science advances (01-03-2021)
    “…Large airbursts, the most frequent hazardous impact events, are estimated to occur orders of magnitude more frequently than crater-forming impacts. However,…”
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