In geoscience we often use ‘quality’ to describe our activities and products, but what does ‘quality’ actually look like? How do we measure it and determine if something is the ‘quality’ facility or ‘quality’ data we say it is? This is not simply an esoteric thought experiment – it matters: end-users and stakeholders are already making decisions potentially affecting whole communities and worth millions of dollars based on their understanding of the quality of our geochemical analytical data. These products are the foundation of Geoscience Australia’s reputation as a trusted advisor to government, communities and industry. This talk will guide you through the Geoscience Australia Laboratory, paying particular focus to our role in quality control and assurance for a range of analytical data products, including our core analytical capabilities in Organic Geochemistry, Microanalysis and Physical Properties. You will hear how the labs are evolving as we build new facilities and build on our capabilities. You will learn more about the importance of quality, how it is defined and some tools to apply in your own work.

Geoscience Australia's value to the nation, outlined in our overarching Strategy 2028, is through our science. However, the way that we apply our science to support a strong economy, resilient society and sustainable environment cannot be taken for granted. Our new Science Strategy 2028, to be launched by Geoscience Australia's Chief Scientist, Dr Steve Hill, during this event, will support Strategy 2028 in our mission to be the nation's trusted advisor on the geology and geography of Australia. It will provide strategic direction for developing and delivering the science that underpins our core business. Dr Hill will outline how our guiding Science Principles apply to our way of working -- not just the way in which we work as an organisation, but also in the way that we work with our partners in using science to create benefits for all Australians.

• Vertical datums are a foundational piece of the positioning puzzle that allows us make sense of height measurements - they make it possible to align height data by defining where all heights are zero. But when the vertical datum is unreliable, we lose perspective on which direction is down and this can cause strange things to happen. Water can appear to flow in the wrong direction or pool in unexpected places. • The Australian Height Datum (AHD) is the current, official, vertical datum in use in Australia. At 50 years old this year, it has stood the test of time well. But, it has a number of bumps and wrinkles (errors and distortions), relies on degrading physical infrastructure and was never intended to be used with modern positioning technology like GPS. The Australian Vertical Working Surface is a shiny new alternative vertical datum that doesn’t depend on any physical infrastructure, is free from the errors in the AHD and is designed to be directly compatible with GPS technology in the first instance.

Studies of three global sediment-hosted zinc provinces (Mt Isa, Australia; Northern Cordillera, Canada/USA; Irish Midlands, Ireland) indicate that deposits in all three provinces are associated with gradients in many geological parameters. These include lead isotopes, the depth of the lithosphere-asthenosphere boundary, upward-continued gravity and magnetotellurics data. These gradients are interpreted to mark major cratonic boundaries, or edges, that control the distribution of these deposits in space and in time. Studies of the Mt Isa Province indicate that regional alteration has caused extensive loss of zinc, copper and cobalt, potentially providing more than sufficient metal for the known deposits. Moreover, in some cases, metal loss corresponds to changes in rock properties, possibly enabling regional mapping of zones of metal loss using geophysical data.

The magnetotellurics (MT) method maps the electrical conductivity/resistivity structure of the subsurface, which provides crucial information for mineral exploration. Geoscience Australia has actively applied the method to provide multiscale world-leading datasets to improve the understanding of geology and resource potential. We demonstrate the value of scaled MT data acquisition starting from mapping large-scale conductivity structures in the lithosphere utilising long-period MT datasets through to the resolution of finer scale structures in the crust suitable for camp scale targeting. Integration of data from multiscale surveys provides an effective way to narrow the search space and to identify ‘targets’ of mineral potential in covered terranes. Our work has helped to increase explorers’ investment confidence for new mineral discoveries in greenfield regions.

The AusAEM survey is the world's largest airborne electromagnetic (AEM) survey flown to date, extending across an area exceeding 3.5 million km2 over Western Australia, the Northern Territory, Queensland, New South Wales Victoria and South Australia. Airborne electromagnetics is a geophysical method at the forefront in addressing the challenge of exploration under cover. In collaboration with the state and territory geological surveys, Geoscience Australia has led a national initiative whose goal is to acquire AEM data at a nominal line spacing of 20 km across Australia. The interpreted AEM conductivity sections were inverted using Geoscience Australia's open source Layered Earth Inversion Sample-By-Sample Time Domain Electromagnetics (GALEISBSTDEM) inversion. Horizontal along-flight line resolution is 12.5 m, and the vertical resolution varies exponentially with depth. Inversion cell sizes increase from 4.0 m at the surface to ~55 m in the bottom cell of the conductivity sections, ~500 m below surface. Consequently, the ability to resolve fine detail varies with depth. Using this dataset, we interpret the depth to chronostratigraphic surfaces, assembled stratigraphic relationship information, and delineated structural and electrically conductive features. Our results improved understanding of upper-crustal geology, led to 3D mapping of palaeovalleys, prompted further investigation of electrical conductors and their relationship to structural features and mineralisation, and helped us continuously connect correlative outcropping units separated by up to hundreds of kilometres. Our interpretation is designed to improve targeting and outcomes for mineral, energy and groundwater exploration, and contributes to our understanding of the chronostratigraphic, structural and upper-crustal evolution of northern Australia. Almost 200,000 regional depth measurements have been collected, each attributed with detailed geological information, are an important step towards a national geological framework, and offer a regional context for more detailed, smaller-scale AEM surveys. The AusAEM programme delivers much more than just reliable depth-to-cover estimates and the location of paleochannels. It can reveal basin architecture and regionally map structures, making it a crucial layer of data for mineral, energy and groundwater and exploration. It has become an essential part of data-driven decision making for conservation and environmental management.

From minerals to meteorites, this presentation will delve into the amazing specimens held at the National Mineral & Fossil Collection, explore our recent work and projects, and identify our diverse stakeholders that we interact with as part of our goals of custodianship, education, outreach, and research support. The National Mineral & Fossil Collection houses world-class mineral, meteorite, fossil, and rock thin-section specimens. The collection is of scientific, historic, aesthetic, and social significance. Geoscience Australia is responsible for the management and preservation of the collection, as well as facilitating access to the collection for research, geoscience education, and public engagement. The collection contains an impressive: • 20,000 gem, mineral and meteorite specimens from localities in Australia and across the globe. • 45,000 published palaeontological specimens contained in the Commonwealth Palaeontological Collection (CPC). • 1,000,000 unpublished fossils in a ‘Bulk Fossil’ collection. • 100,000 rock thin section slides. • 200 historical geoscience instruments including, cartography, geophysical, and laboratory equipment.

Precise positioning based on constellations of navigation satellites brings significant economic and social benefits to Australia. Precise positioning reduces fertiliser and chemical spray waste in agriculture. It improves the efficiency of operations in large mine sites. Precise positioning improves safety in aircraft operations and can even give added freedom of movement to sight impaired people. The rationale behind the Ginan project is to develop the software and data products to allow everybody in Australia to enjoy the benefits of precise positioning through the creation of new services and products, and in doing so drive economic growth enhancing Australia's prosperity.

Australia as it exists today is a product of geological processes that have occurred over its 4.5 billion year history. Isotopic studies are one approach to understanding the history and evolution of the Australian continent. Isotope geochronology tells us about the timing of a wide range of geological processes like crystallisation, deformation and cooling of rocks. Isotope geochemistry informs on the precursor components from which the rocks formed, and can act as 'paleogeophysical' sensors to tell us more about the subsurface. The Isotopic Atlas of Australia brings together five of the most widely used isotopic systems in geology and delivers publicly available maps and datasets in a consistent format. This work is unlocking the collective value of decades of investment in data collection, and facilitating qualitative and quantitative comparison and integration with other datasets such as geophysical images. This talk will be an introduction to the world of isotopes as applied to understand geology, and an overview of the Isotopic Atlas recently produced as part of the Exploring for the Future Program.

The clean energy transition will require a vast increase in metal supply, yet discoveries of new mineral deposits are declining. Recently, several case studies have demonstrated links between electrical conductors imaged using magnetotelluric (MT) data and mineral deposits. Use of MT methods for exploration is therefore growing but the general applicability has not yet been tested. We look at spatial relationships between conductors and three deposit styles and find that volcanic hosted massive sulfide (VHMS) and copper porphyry deposits show weak to moderate correlations with conductors in the upper mantle. In contrast, orogenic gold deposits show strong correlations with mid-crustal conductors. These differences likely reflect differences in the way these deposits form, and suggest a metamorphic-fluid source for orogenic gold is significant. The resistivity signature can be preserved for hundreds of millions of years, and therefore MT can be a powerful tool for mineral exploration.