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    Number of items: 6.

    Chemical Geology

    Seghedi, I. and Bojar, A.V. and Downes, Hilary and Rosu, E. and Tonarini, S. and Mason, P.R.D. (2007) Generation of normal and adakite-like calc-alkaline magmas in a non-subductional environment: An Sr-O-H isotopic study of the Apuseni Mountains neogene magmatic province, Romania. Chemical Geology 245 (1-2), 70 - 88. ISSN 0009-2541.

    Downes, Hilary and Reichow, M.K. and Mason, P.R.D. and Beard, Andrew and Thirlwall, M.F. (2003) Mantle domains in the lithosphere beneath the French Massif Central: trace element and isotopic evidence from mantle clinopyroxenes. Chemical Geology 200 (1-2), pp. 71-87. ISSN 0009-2541.

    Journal of Petrology

    Downes, Hilary and MacDonald, R. and Upton, B.G.J. and Cox, K.G. and Bodinier, J.L. and Mason, P.R.D. and James, D. and Hill, P.G. and Hearn, B.C. (2004) Ultramafic xenoliths from the Bearpaw Mountains, Montana, USA: evidence for multiple metasomatic events in the lithospheric mantle beneath the Wyoming craton. Journal of Petrology 45 (8), pp. 1631-1662. ISSN 0022-3530.

    Lithos

    Beard, Andy and Downes, Hilary and Mason, P.R.D. and Vetrin, V.R. (2007) Depletion and enrichment processes in the lithospheric mantle beneath the Kola Peninsula (Russia): Evidence from spinel lherzolite and wehrlite xenoliths. Lithos 94 (1-4), 1 - 24. ISSN 0024-4937.

    Tectonophysics

    Seghedi, I. and Maţenco, L. and Downes, Hilary and Mason, P.R.D. and Szakács, A. and Pécskay, Z. (2011) Tectonic significance of changes in post-subduction Pliocene–Quaternary magmatism in the south east part of the Carpathian–Pannonian Region. Tectonophysics 502 (1-2), pp. 146-157. ISSN 0040-1951.

    Seghedi, I. and Maţenco, L. and Downes, Hilary and Mason, P.R.D. and Szakács, A. and Pécskay, Z. (2010) Tectonic significance of changes in post-subduction Pliocene-Quaternary magmatism in the south east part of the Carpathian-Pannonian Region. Tectonophysics 502 (1-2), pp. 146-157. ISSN 0040-1951.

    This list was generated on Sat Nov 23 07:01:54 2024 GMT.