Search Results - "Dorais, M.J."

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  1. 1

    Depositional provenance of the Himalayan metamorphic core of Garhwal region, India: Constrained by U–Pb and Hf isotopes in zircons by Spencer, C.J., Harris, R.A., Dorais, M.J.

    Published in Gondwana research (01-07-2012)
    “…U–Pb and Hf isotopes in zircon from the highly metamorphosed core of the Himalaya in the Garhwal region of India indicate that the ortho- and paragneiss units…”
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    Journal Article
  2. 2

    Post-collisional lamprophyric event in Sierra Norte, Córdoba, Argentina: Mineralogical, geochemical and isotopic characteristics by O’Leary, M.S., Lira, R., Dorais, M.J., Tassinari, C.C.G.

    Published in Journal of South American earth sciences (01-10-2009)
    “…Over 20 lamprophyre dykes, varying in width between a few centimeters and several meters, have been identified in central Sierra Norte – Eastern Pampean…”
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    Journal Article
  3. 3

    Analysis of sulfides in whole rock matrices by elemental analyzer–continuous flow isotope ratio mass spectrometry by Studley, S.A, Ripley, E.M, Elswick, E.R, Dorais, M.J, Fong, J, Finkelstein, D, Pratt, L.M

    Published in Chemical geology (16-12-2002)
    “…Potential matrix effects in the sulfur isotopic analysis of whole rocks by elemental analyzer–continuous-flow isotope ratio mass spectrometry (EA–CFIRMS) have…”
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  4. 4

    Fluid–rock interaction at the roots of an Eopaleozoic epithermal system, Sierra Norte de Córdoba, Argentina: Paragenesis, thermometry and fluid sources by Lira, R., Poklepovic, M.F., Dorais, M.J., Millone, H.A., Gomez, G.M.

    Published in Journal of South American earth sciences (01-10-2009)
    “…A deep epithermal vein system hosted in Late Proterozoic to Cambrian granodiorite has been identified in the Sierra Norte de Córdoba, the easternmost range of…”
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  5. 5

    Mineralogy and petrology of cretaceous subsurface lamproite sills, southeastern Kansas, USA by Cullers, R.L., Dorais, M.J., Berendsen, P., Chaudhuri, S.

    Published in Lithos (01-09-1996)
    “…Cores and cuttings of lamproite sills and host sedimentary country rocks in southeastern Kansas from up to 312 m depth were analyzed for major elements in…”
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