Works matching AU Ceuleneer, Georges
Results: 26
Complex tectono-magmatic interaction in the evolution of the George V Transform Fault, South-East Indian Ridge, 140°E, and implications for mantle dynamics.
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- Geophysical Research Abstracts, 2019, v. 21, p. 1
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Origin of Moho: dunite is the Rosetta stone between seismologists and geologists?
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- Geophysical Research Abstracts, 2018, v. 20, p. 2160
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Primitive layered gabbros from fast-spreading lower oceanic crust.
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- Nature, 2014, v. 505, n. 7482, p. 204, doi. 10.1038/nature12778
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Tracing Carbonate Formation, Serpentinization, and Biological Materials With Micro‐/Meso‐Scale Infrared Imaging Spectroscopy in a Mars Analog System, Samail Ophiolite, Oman.
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- Earth & Space Science, 2021, v. 8, n. 11, p. 1, doi. 10.1029/2021EA001637
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The nature of the Moho beneath fast‐spreading centers: Evidence from the Pacific plate and Oman ophiolite.
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- Island Arc, 2022, v. 31, n. 1, p. 1, doi. 10.1111/iar.12460
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The oceanic substratum of Northern Luzon: Evidence from xenoliths within Monglo adakite (the Philippines).
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- Island Arc, 2007, v. 16, n. 2, p. 276, doi. 10.1111/j.1440-1738.2007.00574.x
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A systematic mapping procedure based on the Modified Gaussian Model to characterize magmatic units from olivine/pyroxenes mixtures: Application to the Syrtis Major volcanic shield on Mars.
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- Journal of Geophysical Research. Planets, 2013, v. 118, n. E8, p. 1632, doi. 10.1002/jgre.20112
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Contrasted hydrothermal activity along the South- East Indian Ridge (130°E-140°E): From crustal to ultramafic circulation.
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- Geochemistry, Geophysics, Geosystems: G3, 2017, v. 18, n. 7, p. 2446, doi. 10.1002/2016GC006683
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The remelting of hydrothermally altered peridotite at mid-ocean ridge by intruding mantle diapirs.
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- Nature, 1999, v. 402, n. 6761, p. 514, doi. 10.1038/990073
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Thermal structure of a fossil mantle diapir inferred from the distribution of mafic cumulates.
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- Nature, 1996, v. 379, n. 6561, p. 149, doi. 10.1038/379149a0
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The Origin of Felsic Intrusions Within the Mantle Section of the Samail Ophiolite: Geochemical Evidence for Three Distinct Mixing and Fractionation Trends.
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- Journal of Geophysical Research. Solid Earth, 2021, v. 126, n. 5, p. 1, doi. 10.1029/2020JB020760
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Seismic structure of an oceanic core complex at the Mid-Atlantic Ridge, 22°19′N.
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- Journal of Geophysical Research. Solid Earth, 2010, v. 115, n. B7, p. n/a, doi. 10.1029/2009JB006943
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The Eastern Makran Ophiolite (SE Iran): evidence for a Late Cretaceous fore-arc oceanic crust.
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- International Geology Review, 2019, v. 61, n. 11, p. 1313, doi. 10.1080/00206814.2018.1507764
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Melt-rock interaction as a factor controlling evolution of chromite and olivine in dunite - case study from the Kukes Massif (Mirdita ophiolite, Albania).
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- Journal of Geosciences, 2024, v. 69, n. 1, p. 49, doi. 10.3190/jgeosci.386
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Experimental diopsidite: Implications for natural diopsidite genesis through fluid-melt-mantle peridotite reaction.
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- Mineralogy & Petrology, 2021, v. 115, n. 5, p. 489, doi. 10.1007/s00710-021-00759-7
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COMPOSITION GRADIENTS IN SILICATE INCLUSIONS IN CHROMITES FROM THE DUNITIC MANTLE-CRUST TRANSITION (OMAN OPHIOLITE) REVEAL HIGH TEMPERATURE FLUID-MELT-ROCK INTERACTION CONTROLLED BY FAULTING.
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- Ofioliti, 2020, v. 45, n. 2, p. 103, doi. 10.4454/ofioliti.v45i2.534
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Geoid and depth anomalies over ocean swells and troughs: Evidence of an increasing trend of the geoid to depth ratio with age of plate.
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- Journal of Geophysical Research. Solid Earth, 1988, v. 93, n. B7, p. 8064, doi. 10.1029/JB093iB07p08064
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Earth science: Mantle mapped in the desert.
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- Nature, 2004, v. 432, n. 7014, p. 156, doi. 10.1038/432156a
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How Does Nodular Chromite Nucleate and Grow? An Integrated Microstructural and Petrological Approach.
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- Journal of Petrology, 2024, v. 65, n. 7, p. 1, doi. 10.1093/petrology/egae061
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Origin of Antecrysts in Igneous Rocks from the Salavat Range (NW Iran): an Explanation for the Geochemical Signature of Potassic Alkaline Rocks.
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- Journal of Petrology, 2021, v. 62, n. 7, p. 1, doi. 10.1093/petrology/egab031
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The Chicken and Egg Dilemma Linking Dunites and Chromitites in the Mantle–Crust Transition Zone beneath Oceanic Spreading Centres: a Case Study of Chromite-hosted Silicate Inclusions in Dunites Formed at the Top of a Mantle Diapir (Oman Ophiolite).
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- Journal of Petrology, 2021, v. 62, n. 4, p. 1, doi. 10.1093/petrology/egab026
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A New View on the Petrogenesis of the Oman Ophiolite Chromitites from Microanalyses of Chromite-hosted Inclusions.
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- Journal of Petrology, 2012, v. 53, n. 12, p. 2411, doi. 10.1093/petrology/egs054
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Characterization of hyperalkaline fluids produced by low-temperature serpentinization of mantle peridotites in the Oman and Ligurian ophiolites.
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- Geochemistry, Geophysics, Geosystems: G3, 2013, v. 14, n. 7, p. 2496, doi. 10.1002/ggge.20147
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Mineralogical assemblages forming at hyperalkaline warm springs hosted on ultramafic rocks: A case study of Oman and Ligurian ophiolites.
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- Geochemistry, Geophysics, Geosystems: G3, 2013, v. 14, n. 7, p. 2474, doi. 10.1002/ggge.20146
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Mapping of an ophiolite complex by high-resolution visible-infrared spectrometry.
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- Geochemistry, Geophysics, Geosystems: G3, 2006, v. 7, n. 8, p. n/a, doi. 10.1029/2005GC001214
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Nature and distribution of dykes and related melt migration structures in the mantle section of the Oman ophiolite.
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- Geochemistry, Geophysics, Geosystems: G3, 2003, v. 4, n. 7, p. n/a, doi. 10.1029/2002GC000354
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