VOLCANO: 3 PhD projects at the Queensland University of Technology, Brisbane Australia,

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 3 PhD projects at the Queensland University of Technology, Brisbane Australia
From: "Scott Bryan" scott.bryan@xxxxxxxxxx
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Applications are invited for 3 PhD projects at the Queensland
University of Technology, Brisbane Australia, starting from July 2010.

Further information on the projects contact Dr David Murphy
david.murphy@xxxxxxxxxx and Dr Scott Bryan scott.bryan@xxxxxxxxxx or
see: http://www.earthworks-jobs.com/geoscience/qut10051.html

Application process: (Applications Open 1 May Start no later than Sept 2010)

The online application is available at http://www.qut.edu.au/research/rhd/

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PhD in Igneous Petrology/Geochemistry

Project Title: Geochemistry, Geochronology & Tectonics for
Research of Hot-Dry Rock Geothermal Systems in Queensland, Australia

Project Summary: Queensland University of Technology, Australia in
collaboration with the Queensland Geothermal Energy Centre of
Excellence, will coordinate a geoscience research program to define
geothermal resources in Queensland.  This fully-funded research
project will use recent advances in mineralogy, trace element/isotope
geochemistry, geochronology, and tectonics to develop innovative
scientific methodologies for geothermal research. This project will
produce a comprehensive regional geochemical (particularly trace
elements and isotopes) and zircon chronochemical dataset for
Queensland igneous rocks. The scientific approach developed in this
project will help to understand the timing, location, cause and
distribution of heat producing igneous rocks in Queensland.  This
project will additionally provide new insights into the
tectonomagmatic evolution of Queensland and the generation of regional
high crustal heat flow zones. The PhD program will be based at the
Queensland University of Technology, and jointly supervised by staff
from the Queensland Geothermal Energy Centre of Excellence and
Queensland Geological Survey.
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PhD in Volcanology/Tectonics

Project Title: Determining the role of magmatism in the rupturing of
continents: The transition from the Sierra Madre Occidental to the
Gulf of California of Mexico


Project Summary: Continental margins produced by the rupturing of
continents yet many of the geological processes involved in the
initiation and evolution of continental margins are poorly understood.
As much as 90% of the world's rifted continental margins have been
characterised by voluminous magmatism during their formation, often
termed Volcanic Rifted Margins, but the location, timing and volume of
this magmatism can vary substantially during the rupturing process. A
recent discovery is that these variations of magma within a rupture or
rift system play a major role in controlling the style of rifting. The
main question of this research project will confront is: “Can
substantial magmatism prior to rupturing affect the rifting process
and be an explanation for abrupt variations in observed rifting
style?” The project will be based in western Mexico in a region of
active rupturing as a natural laboratory where the rift extends across
regions with and without substantial pre-rift magmatism. This research
will look at the causal effects of the magmatism, and critically, to
see what the main differences are between volcanic and non-volcanic
rifts and margins. Important outcomes will be identifying the
significant feedbacks magmatism has on rift processes and structure,
basin architecture, evolution and resource potential.

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PhD in Geochemistry

Project Title: Radiogenic isotope (Sr, Nd, Pb & He) analysis of
basaltic samples from the Shatsky Rise. Testing the Plume versus plate
origin for Oceanic Plateaus.

Project Summary: The Shatsky Rise is a large volcanic plateau in the
northwest Pacific that formed ~140Ma in a relatively short time period
on the Pacific oceanic crust. Magnetic lineations in the oceanic crust
indicate that the plateau formed along the trace of a triple junction
of oceanic spreading ridges. This makes Shatsky the ideal location to
test a deep mantle plume origin versus a shallow plate boundary
formation for oceanic plateaus.

The objective of the project is to use Sr, Nd, Pb & He isotope data of
basaltic samples from three of the drill holes that intersected
igneous basement during IODP Expedition 324 to characterise the nature
and origin of the mantle material that melted to form the plateau
volcanism of the Shatsky Rise.

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