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Développement et migration du magma granitique, Wuluma Hills, Australie Centrale /Dombrowski, Clément, January 1997 (has links)
Mémoire (M.Sc.T.)--Université du Québec à Chicoutimi, 1997. / Document électronique également accessible en format PDF. CaQCU
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Petrology of the Deer Isle Pluton, coastal Maine : a complex mixed magma system /Hooks, Benjamin Patrick. Lux, Daniel R. January 2003 (has links)
Thesis (M.S.) in Geological Sciences--University of Maine, 2003. / Includes vita. Includes bibliographical references (leaves 131-140).
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Magmatic enclaves and evidence for magma mixing in the Oak Point Granite, Deer Isle, Maine, U.S.A. /Johnston, Ben. January 2001 (has links)
Thesis (M.S.) in Geological Sciences--University of Maine, 2001. / Includes vita. Includes bibliographical references (leaves 105-110).
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On the architecture of magmatic crystal mushSmith, Graham Christopher January 2010 (has links)
No description available.
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Mixing processes in shallow magma chambersCowan, Alexander Hayden Kennedy January 2012 (has links)
No description available.
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Temporal magma dynamics during solidification of the mafic-silicic complex of Isle de Haut, MainePatwardhan, Kaustubh, January 2009 (has links) (PDF)
Thesis (Ph. D.)--Johns Hopkins University, 2009. / Vita. U.M.I. no. 3356981. Title from PDF title page (viewed on May 24, 2010) Available through UMI ProQuest Digital Dissertations. Includes bibliographical references (l. 136-145). Also issued in print.
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Solitary wave solutions for the magma equation: symmetry methods and conservation lawsMindu, Nkululeko 30 January 2015 (has links)
A dissertation submitted for the degree of Masters of Science, School of Computational and Applied Mathematics, University of Witwatersrand, Johannesburg, 2014. / The magma equation which models the migration of melt upwards through
the Earth’s mantle is considered. The magma equation depends on the permeability
and viscosity of the solid mantle which are assumed to be a function
of the voidage . It is shown using Lie group analysis that the magma equation
admits Lie point symmetries provided the permeability and viscosity satisfy
either a power law, or an exponential law for the voidage or are constant. The
conservation laws for the magma equation for both power law and exponential
law permeability and viscosity are derived using the multiplier method.
The conserved vectors are then associated with Lie point symmetries of the
magma equation. A rarefactive solitary wave solution for the magma equation
is derived in the form of a quadrature for exponential law permeability and viscosity.
Finally small amplitude and large amplitude approximate solutions are
derived for the magma equation when the permeability and viscosity satisfy
exponential laws.
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Advanced argillic and sericitic alteration in the Buckskin Range, Nevada : a product of ascending magmatic fluids from the deeper yerington porphyry copper environment /Lipske, Joanna L. January 2002 (has links)
Thesis (M.S.)--Oregon State University, 2003. / Includes folded maps in pocket. Typescript (photocopy). Includes bibliographical references. Also available online.
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Convection of magma in volcanic conduits as a degassing mechanism at active volcanoes /Witter, Jeffrey Bruce. January 2003 (has links)
Thesis (Ph. D.)--University of Washington, 2003. / Vita. Includes bibliographical references (leaves 235-250).
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Geochemistry of neoproterozoic arc-related plutons in the Western margin of the Yangtze Block, South ChinaZhao, Junhong, January 2008 (has links)
Thesis (Ph. D.)--University of Hong Kong, 2008. / Includes bibliographical references (leaf 304-311) Also available in print.
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