GEMOC ARC National Key Centre

Industry interaction

 

 

INDUSTRY INTERACTION, TECHNOLOGY TRANSFER AND COMMERCIALISATION PROGRAM

GEMOC relies on a vigorous interaction with the mineral exploration industry at both the research and the teaching/training levels.  The research results of the Centre’s work are transferred to the industry and to the scientific community by:

• collaborative industry-supported Honours, MSc and PhD projects

• short courses relevant to the industry and government sector users, designed to communicate and transfer new technologies, techniques and knowledge in the discipline areas covered by the Key Centre

•  one-on-one research collaborations and shorter-term collaborative research on industry problems involving national and international partners

•  provision of high quality geochemical analyses with value-added interpretations in collaboration with industry and government organisations, extending our industry interface

•  use of AccessMQ consultancies and collaborative industry projects, which employ and disseminate the technological developments carried out by the Centre

•  GLITTER, an on-line data-reduction program for Laser Ablation ICPMS analysis, developed by GEMOC and CSIRO GEMOC participants, has been successfully commercialised and is available from GEMOC through AccessMQ (http://www.es.mq.edu.au/GEMOC/); the software is continuously upgraded

•  collaborative relationships with technology manufacturers (more detail in the section on Technology Development). GEMOC (Macquarie) is the Australian demonstration site for Agilent Technologies LAM-ICPMS applications

 

SUPPORT SOURCES

GEMOC industry support includes:

•  direct funding of research programs

•  "in kind" funding including field support (Australia and overseas), access to proprietary databases, sample collections, digital datasets and support for GIS platforms

•  logistic support for fieldwork for postgraduate projects

•  collaborative research programs through ARC Linkage Projects and the Macquarie University External Collaborative Grants (MUECRG) and PhD program support

•  assistance in the implementation of GIS technology in postgraduate programs

•  participation of industry colleagues as guest lecturers in undergraduate units

•  extended visits to Macquarie by industry personnel for interaction and research

•  ongoing informal provision of advice and formal input as members of the Advisory Board

 

ACTIVITIES IN 2009

4 Industry Reports were completed for collaborative industry projects.

TerraneChron^® studies (see Research Highlights) have enjoyed continued uptake by a significant segment of the global mineral exploration industry. This methodology, currently unique to GEMOC, requires the integration of data from three instruments (electron microprobe, LAM-ICPMS and LAM-MC-ICPMS) and delivers fast, cost-effective information on the tectonic history (with ages) of regional terranes (www.gemoc.mq.edu.au/TerraneChron.html).

The ARC Linkage Project titled “Global Lithosphere Architecture Mapping” (GLAM) continued with full industry partner support following the takeover of WMC Resources by BHP Billiton. A successful bid for an ARC Linkage grant in 2008 ensured the continuation of the project despite key players leaving BHP Billiton. A sub-licencing agreement was executed with Minerals Targeting International to accommodate Dr Graham Begg's new role (in relationship to Macquarie, BHPB and the GLAM project) as Director of this company. Planning and workshop sessions at Macquarie with participants from BHP Billiton and GEMOC were key activities in 2009. Dr Begg spent significant research time at GEMOC through 2009 as part of the close collaborative working pattern for this project.

GLAM participants visited for several days to discuss results from the ARC Linkage Project Back row (L-R): Nic Rosengren (BHP Billiton), Sue O'Reilly, Bill Griffin, Craig O'Neill, Elena Belousova, Lev Natapov, Norm Pearson, Graham Begg and Juan Carlos Afonso..

 

Graham Begg was the Society of Economic Geologists International Exchange Lecturer for 2009. The role of the lecturer is to share insights involving research into ore deposit science and/or exploration methodology. A total of 34 talks in 8 countries were given to groups of geoscientists from academia, industry and government and highlighted GEMOC's GLAM project. Talks focused on the relationships between planet- and lithosphere- scale processes, lithospheric architecture and composition, geodynamic history, and ore deposit genesis in space and time.

GEMOC's development of a method to analyse trace elements in diamond has opened up potential further developments and applications relevant to industry, ranging from diamond fingerprinting for a range of purposes to improving the knowledge framework for diamond exploration. An ARC Linkage Project on Diamond Fingerprinting supported by Rio Tinto finished in mid-2009 with a final report. Dr Debora Araujo was employed as a Research Associate on the project and has carried out an extensive program of method development and diamond analysis.

In 2007-2008 GEMOC developed a technique for dating the intrusion of kimberlites and lamproites using LAM-ICPMS U-Pb analysis of groundmass perovskite (see GEMOC Publication #505). This rapid, low-cost application has proven very attractive to the diamond exploration industry, and has led to several small collaborative projects; it also is being applied in a new ARC Linkage project sponsored by De Beers.

During 2009, GEMOC increased its collaboration with CERCAMS, the Centre for Russian and Central EurAsian Mineral Studies at the Natural History Museum, London, that serves the international mineral deposits community as a centre for research into the geodynamics and metallogenesis of the Former Soviet Union and neighbouring territories. The final report entitled "Western Altaids Module 2: Hf-Isotope Data" was delivered to CERCAMS in March, 2009 and the results were presented for the industry collaborators at the Final Reporting Meeting CERCAMS Altaids Project Module-2 at the University of Toronto in February 2009.

During 2009 a new initiative was the application of U-series isotopes to the investigation of groundwater studies for both exploration and investigation of palaeoclimate. Collaboration with Heathgate Resources at the Beverley Uranium mine in South Australia has investigated these processes using a well constrained aquifer system in both a mining and exploration context.

Modelling capabilities have now been extended to industry related projects. An ongoing collaboration with Granite Power Ltd continues, which has led to important data exchange and ongoing consulting projects through AccessMQ. An Honours project funded by Chevron Australia Ltd. is underway, studying the thermal evolution of the Carnarvon Basin, and Chevron is covering the direct costs of the project (data acquisition and processing, flights to Western Australia and accommodation for student and supervisor). An ongoing collaboration with Hydrolex Ltd. has also led to important data exchange across the Sydney Basin region.

Studies on the controls of fractionation and concentration of platinum-group elements (PGE) in ultramafic magmas continued in 2009 as part of PhD project of Marek Locmelis, funded by AMIRA Project P710a. The research goal is to develop reliable geochemical indicators that can guide the exploration for magmatic nickel-sulfide deposits with a particular focus on the role of chromite and olivine in the concentration and fractionation of PGE in komatiites. Industry partners are BHP Billiton, Independence Group NL, Norilsk Nickel, MERIWA and ARC. The project is in collaboration with the Centre for Exploration Targeting / University of Western Australia, CSIRO Exploration and Mining and the Australian National University.

 

Archean lava lake outcrop from Marek Locmelis' PhD field area at Kurrajong, Western Australia (see Research Highlight).

 

A continuing collaborative research relationship with New South Wales Geological Survey is applying TerraneChron^® to investigations of the provenance of targeted sequences in Paleozoic sedimentary terranes of eastern Australia, and the development of the Macquarie Arc.

Industry visitors spent varying periods at GEMOC in 2008 to discuss our research and technology development (see visitor list, Appendix 3). This face-to-face interaction has proved highly effective both for GEMOC researchers and industry colleagues.

DIATREEM continued to provide LAM-ICPMS analyses of garnets and chromites to the diamond-exploration industry on a collaborative basis.

GEMOC publications, preprints and non-proprietary reports are available on request for industry libraries.

GEMOC was prominent in delivering keynote and invited talks and workshop modules at national and international industry peak conferences in 2009, including 2 Plenary Addresses. Sue O'Reilly was a member of the organising committee for the SGA Conference in Townsville in 2009. See Appendix 4 for abstract titles and GEMOC Publications.

A new collaborative research project aimed at developing an integrated approach to understanding the formation of mineral sand deposits using Australian deposits as a world benchmark, and to improve exploration strategies employed in Australia and in Russia was initiated in collaboration with Professor Alexandr Kremenetsky from Institute of Mineralogy, Geochemistry and Crystal Chemistry of Rare Elements (IMGRE), PIRSA and Iluka Resources. The results were discussed during the meeting at the Iluka Resources office in Adelaide in August, 2009 and presented at the 13th IAGOD Symposium, Adelaide 2010.

A new collaborative research project was started with the Geological Survey of Western Australia, in which GEMOC is carrying out in-situ Hf-isotope analyses of previously SHRIMP-dated zircon grains from across the state. This is a part of the WA government's Exploration Incentive Scheme.

 

CURRENT INDUSTRY-FUNDED COLLABORATIVE RESEARCH POJECTS

 

These are brief descriptions of current gemoc projects that have direct cash support from industry with either formal ARC or Macquarie University Grant status, and timeframes of at least one year. Projects are both national and global. In addition to these formal projects, many shorter projects are directly funded by industry alone, and the results of these feed into our basic research database (with varied confidentiality considerations). Such projects are administered by AccessMQ, Macquarie’s commercial entity.

GEMOC’s industry collaborative projects are designed to develop the strategic and applied aspects of the basic research programs based on understanding the architecture of the lithosphere and the nature of Earth’s geodynamic processes that have controlled the evolution of the lithosphere and its important discontinuities. Most of the industry collaborative projects rely on geochemical information from the Geochemical Analysis Unit in GEMOC and especially on novel methodologies developed by (and some unique to) GEMOC.

Geochemical data on crustal and mantle rocks are being integrated with tectonic analyses and large-scale datasets (including geophysical data) to understand the relationship between lithosphere domains and large-scale mineralisation.

The use of mantle sulfides to date mantle events, and the characterisation of crustal terrane development using U-Pb dating and Hf isotopic compositions of zircons provide more information for integration with geophysical modelling. TerraneChron^® (see Research Highlights) is an important tool for characterising the tectonic history and crustal evolution of terranes on the scale of 10 – 100 km and delivers a cost-effective exploration tool to the mineral (and potentially petroleum) exploration industry.

The recent breakthrough in developing a robust methodology to analyse the trace elements in diamonds quantitatively is another world-first for GEMOC. In addition to providing unique knowledge about the nature and compositions of deep mantle fluids that has led to a new hypothesis for how diamonds form in the Earth’s mantle (see Research highlights 2007), it has potential practical applications to diamond fingerprinting for forensic applications and to better prediction of targets for diamond exploration.

 

Formal projects known to be funded for 2009:

A novel approach for economic uranium deposit exploration and environmental studies Supported by ARC Linkage Industry Collaborator: Heathgate Resources Summary: The project proposes the use of a novel approach to prospect for economic uranium ore deposits. The measurement of radioactive decay products of uranium in waters (streams and aquifers) and sediments will allow us to (i) identify and locate economic uranium ore deposits and (ii) quantify the rate of release of uranium and decay products during weathering and hence the evolution of the landscape over time. In addition, this project will improve our knowledge of the mobility of radioactive elements during rock-water interaction, which can be used to assess the safety of radioactive waste disposal. Outcomes of this project will be: (i) the discovery of new economic uranium deposits; (ii) development of a new exploration technology allowing for improved ore deposit targeting. Information gained on the behaviour of radioactive elements at the Earth's surface will be critical for the study of safety issues related to radioactive waste storage and obtaining reliable time constraints on the evolution of the Australian landscape.

 

Formal projects commencing 2009: 

Composition, structure and evolution of the lithospheric mantle beneath southern Africa: improving area selection criteria for diamond exploration Supported by ARC Linkage Industry Collaborator: De Beers Summary: Trace-element analyses of garnet and chromite grains from kimberlites distributed across the Kaapvaal craton and the adjacent mobile belts will be used to construct 2D and 3D models of compositional and thermal variation in the lithospheric mantle (to ~250km depth), in several time slices. Regional and high-resolution geophysical datasets (e.g. seismic, magnetotelluric, gravity) will be used to test and refine this model. Links between changes in the compositional structure of the lithospheric mantle and far-field tectonic events will be investigated using 4-D plate reconstructions. The results will identify factors that localise the timing and distribution of diamondiferous kimberlites, leading to new exploration targeting strategies.

 

 

 

Global Lithosphere Architecture Mapping II Summary: Supported by ARC Linkage Industry Collaborator: BHP Billiton Summary: Domains of different composition in the deep part of Earth’s rigid outer shell (the lithosphere) reflect processes of continent formation and breakup through Earth’s history. These boundaries focus the fluid flows from the deeper convecting mantle that may produce giant ore deposits. We will integrate mantle petrology, tectonic syntheses, and geophysics to image the 3-D architecture of the continental lithosphere, and provide a basis for realistic dynamic modelling of the behaviour of these deep continental roots and their response to geodynamic forces through time. This will provide a new approach to identifying predictive relationships between different types of lithosphere domains and structures, and large-scale mineralisation. The continents have been broken up and re-assembled along major zones of weakness many times through Earth’s history. Boundaries between such continental domains focus large-scale movements of fluids that can produce giant ore deposits. This study will provide new perspectives on the localisation of world-class economic deposits, the Earth resources on which society depends.

 

 

 

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