The University of Melbourne
The University of Melbourne  
 

A Selection of Current Research Topics

Contact supervisors for further information...

 


Lake Baikal, Russia

Thermochronology, Geochronology & Tectonics

Masters projects:

Thermochronology and Provenance of the Upper-Palaeozoic Mansfield Basin using fission track and U/Th-He dating of detrital apatites and zircons

Supervisor: Prof. Andrew Gleadow

Dating of Cainozoic volcanic rocks of eastern Australia by the U/Th-He method applied to zircon megacrysts in lavas U/Th-He thermochronology of the early Cretaceous Otway Group in southwestern Victoria

Supervisor: Prof. Andrew Gleadow

Thermochronology and neotectonics of the Mornington Peninsula/King Island high

Supervisor: Prof. Andrew Gleadow

The effect of accumulated radiation damage on the helium retentivity of Sphene and zircon

Supervisor: Prof. Andrew Gleadow

PhD Projects:

Fission track and U/Th-He Thermochronology and sediment mass balance in coupled drainage-basins and sedimentary depocentres

Supervisor: Prof. Andrew Gleadow

The long-term evolution of land surfaces in Precambrian shield areas using integrated quantitative dating and thermochronology techniques

Supervisor: Prof. Andrew Gleadow

Development of automated image analysis for fission track dating and thermochronology in natural minerals

Supervisor: Prof. Andrew Gleadow

Integrated U/Th-He and Fission track thermochronology and the morphotectonic evolution of landscapes adjacent to the east African Rift System

Supervisor: Prof. Andrew Gleadow

U/Th-He thermochronology and the tectonic and denudation history of metamorphic core complexes in the Basin and Range Province of southwestern North America

Supervisor: Prof. Andrew Gleadow

Vertical thermochronologic profiles in orogenic belts from U/Th-He analyses of apatites and the interpretation of tectonic and surface process rates

Supervisor: Prof. Andrew Gleadow

Investigation of the U/Th-He systematics of uranium-bearing accessory minerals

Supervisor: Prof. Andrew Gleadow

The neotectonic history of southeastern Australia from (U-Th)/He apatite thermochronometry

Supervisor: Dr Barry Kohn

The tempo of rhyolitic volcanism in Taupo Volcanic Zone, New Zealand from (U-Th)/He numerical dating

Supervisor: Dr Barry Kohn

An integrated approach to quantifying rates of escarpment retreat using in-situ-produced cosmogenic isotopes and low temperature thermochronologic data

Supervisor: Dr Roderick Brown

Modelling and visualising the evolution of continental landscapes over geological time scales

Supervisors: Dr Roderick Brown & Prof. Andrew Gleadow

 


Pilansberg, South Africa
Isotope Geochemistry & Petrology

Lu-Hf isotope constraints on crust-mantle evolution

For many years isotopic analysis has formed the cornerstone of studies of crust and mantle evolution. Now the development of new analytical technologies (multi-collector ICPMS) offers the opportunity of exploiting the previously under-utilised Lu-Hf decay system to provide important new information. This project will incorporate both bulk rock and in-situ laser ablation studies of a variety of sample suites.

Supervisors: Drs Jon Woodhead & Janet Hergt

Petrogenetic studies of S-type Lachlan Fold Belt granites:

I. The Strathbogie Batholith and Violet Town Volcanics

In addition to key geochemical, geophysical and tectonic characteristics, the common association/preservation of felsic volcanics with granite magmatism in the Melbourne Zone is unusual. This project will combine field and geophysical information, together with state-of-the-art geochemical data (including isotope and trace element geochemistry) to unravel the petrogenesis of the Strathbogie Batholith and associated Violet Town Volcanics.

Supervisors: Drs Janet Hergt & Neil Phillips (CSIRO)

II. The petrogenesis of the Geehi Suite

Enclave-rich S-type granites of the Geehi Suite are located in southern NSW in the vicinity of Tallangatta, and carry abundant inclusions encompassing a wide range of lithologies, presumably entrained from the magma source region. Excellent exposures of this granite have been documented that provide unparalleled opportunities to investigate the source and evolution of S-type granites of the Lachlan Fold Belt. This project will require detailed mapping, sampling and application of petrographic, major, trace element and isotope geochemical techniques to both enclave and host granite lithologies.

Supervisors: Drs Janet Hergt & Jon Woodhead


Cosmogenic isotopes and crustal recycling

It is now almost 20 years since the cosmogenic isotope 10Be was first discovered in the erupted products of convergent margin volcanoes, providing conclusive evidence for subduction of sedimentary material deep into the Earth's mantle. Since then, however, very few further studies have been conducted despite considerable advances in our understanding of subduction zone processes. This project combines outstanding sample materials with the excellent facilities available in the cosmogenic isotope laboratory in an attempt to address critical unsolved issues in island arc petrogenesis, and their relevance to global geochemical cycles.

Supervisors: Drs Jon Woodhead, Janet Hergt, & Rod Brown


Direct dating of mineralisation using Pb-Pb step-leaching geochronology

Pb-Pb step-leaching is a recently developed analytical technique, allowing the dating of individual mineral phases by leaching of radiogenic Pb from the lattice in progressively stronger acids. We have already applied this method to metamorphic minerals such as garnet and staurolite from the Broken Hill region with excellent results. Studies in other laboratories worldwide are now indicating that the technique can be adapted to dating ore genesis using a variety of phases such as sulphides (e.g., pyrrhotite, pyrite, molybdenite) and tourmaline. This project seeks to undertake pilot studies in order to establish the applicability of this emerging technology to the Australian environment.

Supervisors: Drs Jon Woodhead & Janet Hergt

The mineralogy, petrology, geochemistry and genesis of ore deposits in Palaeoproterozoic rift settings and their analogues in Tertiary-Recent settings

Special emphasis on submarine hydrothermal base metal systems and epithermal equivalents.

Supervisor: Prof. Ian Plimer

 


McDonnell Ranges, Australia

Structural Geology & Metamorphism

Study in Proterozoic Orogenic zones

To establish the timing, kinematic and metamorphic relationships within the major faults and shear zones that transect selected areas in the east Antarctica shield and the Gawler Craton in the Eyre Peninsular, South Australia. Planar and linear fabric elements and their kinematic significance will be related to the folds and lineation development outside the areas of high strain. To combine this with information from metamorphic assemblages and age dating to establish pressure-temperature-time paths for the orogenies involved and intrusive events. NB Any work on Antarctic projects is subject to Antarctic Scientific Advisory Committee approval and applicants passing the appropriate medical examinations.

Supervisors: Prof. Chris Wilson & Assoc. Prof. Roger Powell

Structural investigation of Antarctic glaciers

A structural investigation will be undertaken of an Antarctic outlet glacier in order to quantify the development of brittle and ductile structures. This will involve the identification and monitoring of zones of fast flowing ice and crevasse fields (as described by Marmo & Wilson 1998; J. Struct. Geol. 20,149-162). It will also involve either numerically or experimentally modelling the processes that act during macro- to microscopic flow and the control this has on the dynamics of ice masses in Antarctica.

Supervisor: Prof. Chris Wilson

The uplift of Antarctica

To establish the timing and thermal histories in relationship to the major structural events in the east Antarctic shield. Using Ar/Ar and Fission track techniques to relate metamorphic cooling histories to crustal vertical sections, both in local profiles and on a regional scale in order to establish the temporal relationships between tectonic terrains at different levels in the earth's crust. This will lead to the development of tectonic models for the orogenies involved and accompanying intrusive events.

Supervisor: Prof. Chris Wilson

Structural evolution of Tibetan Plateau, China

To establish the structural-metamorphic and timing and relationships between the major faults and shear zones that form the eastern boundary of the Tibetan Plateau. In particular to establish the kinematic significance of the Himalayan events that are superimposed on the late Triassic Indosinian Orogeny. This will involve undertaking field investigations of a folded Triassic accretionary sequence, followed by detailed geochronological analyses of rocks and minerals. This has important implications for how continental margins evolve, particularly as it applies to Asian collisional tectonics.

Supervisor: Prof. Chris Wilson

Structural and tectonic evolution of the east Antarctic shield

The east Antarctic shield has formed a central cratonic block within the two most recent cycles of supercontinent growth and dispersion, ie. the formation of Rodinia and Gondwana. The thrust of the project will be to unravel the structural and metamorphic evolution in the rocks outcropping in selected areas of Prydz Bay and Prince Charles Mountains, and geochronologically constrain these events using modern U-Pb and Ar-Ar geochronology, coupled with thermodynamic metamorphic modelling. With an aim to understand the deformation-pressure-temperature-time evolution of the terrain that has applications to continental scale correlations with adjacent continents.

Supervisors: Prof. Chris Wilson & Assoc. Prof. Roger Powell

Structural, mineralogical and fluid flow related to gold mineralisation

Gold mineralisation in the central Victorian gold fields is controlled on a scale of kilometres to metres by the location of folds, faults and quartz veins. These structures can act as pathways for gold-bearing fluids. This study will involve both field investigations and computer modelling to understand the control that structure exerts on the location of the greatest fluid flow. By identifying the mineralogical assemblages, in quartz veins, with numerical quantification of fluid phases and mechanical interactions in the deforming region, it will be possible to gain an insight into the importance of deformation-induced fluid-flow.

Supervisor: Prof. Chris Wilson

Dating the mineralising system in western Victoria

This will involve establishing the timing and kinematic relationships between the major structural events, metamorphic/alteration assemblages to mineralisation in western Victoria. Ar-Ar, U-Th-He and Fission Track dating techniques will be used to establish temperature-deformation-time paths for the orogenies involved and the accompanying intrusive and mineralising events. Such information will also be related to the exhumation and unroofing of mineralised systems in southeastern Australia.

Supervisors: Dr David Phillips & Prof. Chris Wilson

Geochemistry and geochronology of fluid inclusion systems related to gold mineralisation in western Victoria

This project is aimed at determining the nature and timing of fluid systems associated with gold mineralisation in western Victoria. The project will involve the development of methods for measuring of halogen (Cl, Br, I) and noble gas compositions as well as Ar-Ar dating of fluid inclusion systems in quartz veins related with gold mineralisation.

Supervisors: Dr David Phillips & Prof. Chris Wilson

Geophysical characterisation of the mineralised systems in western Victoria

This will involve relating crustal rock associations and structures to sub-surface geophysical data namely gravity and magnetic data sets. Aeromagnetic anomalies will be related to mineralisation processes by empirical and theoretical rock-magnetic (magnetic petrophysics) studies of rocks form mineralised versus non-mineralised areas and to obvious fluid migration pathways. Predictive models of aeromagnetic and downhole magnetic textures leading directly to orebody detection, beyond the current indirect interpretation of aeromagnetics will be developed as a regional exploration tool.

Supervisors: Dr Bob Musgrave (La Trobe University) & Prof. Chris Wilson

Fluid flow and structural modelling of gold deposits in China

This project will be centred on mineralised sites in Yunan, China in order to understand the structural and stratigraphic controls on gold deposition from fluids within a Carlin-type gold deposits. An important aspect of this project will be to understand how the ore deposit is intimately related to the physical and chemical character of the host rocks, fluid composition, source, migration paths and deposition sites. The project will involve modelling the system at a number of scales to understand the localisation of mineralisation within the fault systems from a mine to regional scale.

Supervisor: Prof. Chris Wilson

 


Ganges Delta, India

Stratigraphy, Sedimentology & Hydrogeology

 

Microfossil biostratigraphy and palaeobathymetry of the Palaeogene petroleum reservoir and capping facies of the Offshore Gippsland Basin

The Late Cretaceous to Eocene Latrobe Group of the Gippsland Basin hosts over 50% of Australia's petroleum reserves, these strata are sealed by the Oligocene to Recent Seaspray Group. The Latrobe Group sediments preserve facies from terrestrial to marine conditions preserving shallow marine shelfal sands and clays which were deposited as a series of sand bars, foraminiferal faunas are present in these facies and have never been described or used for palaeoenvironmental studies of the reservoir facies. The overlying Palaeogene Seaspray Group sediments consist of shelfal to bathyal marls forming a seal on the Latrobe Group. This project will use microfossils, facies and wireline log analyses together with core, sidewall core and cutting samples to achieve the following:

(1) To constrain the palaeoenvironmental evolution of the Latrobe Group marine facies.

(2) To data key marine reservoir sequences and using foraminiferal assemblages with other facies data and wireline logs and/or seismic data correlate these marine events.

Supervisor: Dr Stephen Gallagher

 

Cretaceous to Early Tertiary foraminiferal palaeoenvironments and stratigraphy of the petroleum prospective strata of the Otway Basin and the evolution of the Southern Ocean

This project will examine the evolution of the Southern Ocean from the time Australia rifted from Antarctica 97 million years ago to 30 million years ago. The research will date marine incursions of this ocean into the southern margin of Australia. Better microfossil age estimates of these Cretaceous to Tertiary incursions will lead to improved correlations of strata hosting economic hydrocarbons in the region. Studies of foraminifera and sedimentary (palaeo)environmental signals preserved in these strata will contribute to understanding oceanic and sea level changes in the Southern Ocean, and help time the opening of the Tasman Rise. The study will utilise foraminiferal data, lithofacies analyses of core and cuttings and wireline logs to:

1. Provide accurate age dating of representative sections of bores and well sequences plus outcrops in the Otway area using foraminifera

2. Determine the palaeoenvironmental evolution of the Cretaceous to Paleocene clasitcs of the offshore Otway Basin using microfossils.

3. Date the first marine incursions into the region, representing the first marine vestages of the now vast Southern Ocean.

Supervisor: Dr Stephen Gallagher

 

The lithostratigraphy and foraminiferal distribution of the Tertiary to Recent carbonates in the Bass Basin Victoria

The aim of this PhD project is to study the stratigraphy the Tertiary carbonate rocks of the Bass basin using seismic lines, wireline logs with outcrop and well samples to establish a stratigraphic framework for the Bass Basin. The Bass Basin is a well explored yet poorly known offshore region of Victoria and there exists a variety of company data that can be researched including a huge sea bed sample database.

Supervisor: Dr Stephen Gallagher

 


Rio Negro, Brazil
Surface Processes & Quaternary Geology

An integrated approach to quantifying rates of escarpment retreat using in-situ-produced cosmogenic isotopes and low temperature thermochronologic data

Supervisor: Dr Roderick Brown

Modelling and visualising the evolution of continental landscapes over geological time scales

Supervisors: Dr Roderick Brown & Prof. Andrew Gleadow

The long-term evolution of land surfaces in Precambrian shield areas using integrated quantitative dating and thermochronology techniques

Supervisor: Prof. Andrew Gleadow

Integrated U/Th-He and Fission track thermochronology and the morphotectonic evolution of landscapes adjacent to the east African Rift System

Supervisor: Prof. Andrew Gleadow

 


Hurricane Mitch 1998, USA
Atmosphere, Oceans & Geophysics

 

The Changes in Extratoprical Cyclone Behaviour under Greenhouse Warming Conditions

Supervisor: Assoc. Prof. Ian Simmonds

Drought and Variations in the Atmospheric Hydrological Budget over Australia

Supervisor: Assoc. Prof. Ian Simmonds

Multidecadal Vacillations in the Climate System in the Antarctic Region

Supervisor: Assoc. Prof. Ian Simmonds

 


Geomicrobiology and Environmental Aqueous Systems

 

Bacterial sulfate reduction in acidic metals-contaminated systems

This project will use molecular microbiological and aqueous/isotope hydrogeochemical approaches to investigating the activity, distribution, geochemical environment, phylogeny and metabolism of sulfate-reducing bacteria (SRB) associated with acid mine/rock drainage systems.  These bacteria tend to be novel, deeply-branching species on the tree of life and may yield insights into geochemical conditions associated with the evolution of bacterial sulfate reduction.  Acid-tolerant SRB are also of high interest to mining/metals recovery and bioremediation projects in which their ability to induce precipitation of a range of precious/toxic metals (as nanometer-scale biominerals) may be harnessed both economically and environmentally.   We will investigate these topics in the context of spatial and temporal variability in surface-/groundwater interactions and how they impact microbial community structure.   For more info, please contact: jmoreau@unimelb.edu.au, and include "SRB project" in subject field to avoid accidental spam filtering.

Supervisor: John Moreau

The biogeochemistry and ecogenomics of microbial mercury methylation

Sulfate- and iron-reducing bacteria have been implicated in the methylation of mercury.  Environmentally, bacterial mercury methylation is the root of global methylmercury contamination in the marine food web.  The speciation of bioavailable mercury for methylation has not yet been determined.  This project will combine a synchrotron-based microanalytical approach (EXAFS) with laboratory pure-culturing experiments to constrain and, hopefully, identify the form of bioavailable mercury in natural sediments and waters, and the mechanism by which it is uptaken by bacteria.  From there, we will attempt to tackle the unresolved problem of the enzymatic pathway by which mercury is methylated in sulfate- and iron-reducers, and the genes underpinning this process.  Ultimately, the goal will be to understand these "mechanistic" systems in the context of field observations, and inversely, be able to predict the methylation potential of natural systems.  For more info, please contact jmoreau@unimelb,edu.au, and include "MeHg project" in the subject field to avoid accidental spam filtering.

Supervisor: John Moreau

 

 

 

 

 

 

School of Earth Sciences : University of Melbourne : Victoria 3010 : AUSTRALIA : Ph: +61 (0)3 8344 7675 : Fax: +61 (0)3 8344 7761
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