Experience

Mira Geoscience

• Canada
• Mining
• 1 - 100 Employee

• Senior Consultant

  • Jul 2019 - Present



Aurora Australis GeoConsulting Pty Ltd

• Mining

• Geophysical and Prospectivity analysis Consultant

  • Mar 2014 - Present

  www.auroraaustralisgeoconsulting.com www.auroraaustralisgeoconsulting.com



Centre for Exploration Targeting

• Adjunct Research Fellow

  • Sep 2012 - Present

  To increase cooperation and activities between the University and leaders and members of academia, professions, business, industry, community, and the public sector, in Australia and overseas.

• Research assistant professor

  • Sep 2009 - Sep 2012

  Aurore Joly was involved in exciting work streams that involved 3D geophysical modelling and prospectivity analysis: i) 4D architecture of West Arunta orogen (+orogenic/intrusive gold, Sedex,surficial/unconformity Uranium)ii) 4D architecture of Paleoproterozoic gold deposit (Tanami, WA) (+ Propectivity analysis on orogenic and intrusive gold)iii) West Musgrave orogen (orogenic/intrusive gold, surficial/unconformity uranium, magmatic nickel-copper-platinum group element, Iron Oxide Copper Gold, granite-hosted tin-tungsten).iv) Capricorn and Gascoyne orogen (+ orogenic/intrusive gold, surficial/unconformity uranium, magmatic nickel-copper-platinum group element, Iron Oxide Copper Gold, diamonds) Show less



Resource Potentials Pty Ltd

• Australia
• Mining
• 1 - 100 Employee

• Senior Consulting Geophysicist and Structural Modeller

  • Jan 2017 - Jun 2019



St Barbara Limited

• Australia
• Mining
• 400 - 500 Employee

• Senior geophysicist

  • Oct 2012 - Jan 2014

  Role accountabilities: i. Providing sound technical advice to the Company’s geoscientists on appropriate geophysical solutions and programs to generate exploration and resource development drill targets and achieve improved mine performance and ore recovery in Australia, the Solomon Islands and Papua New Guinea. ii. Management of continuing programs of geophysical surveys, data acquisition, interpretation and data integration within the Company’s exploration and operational projects. iii. Actively engaging and managing geophysical contractors for safe and efficient completion of data acquisition programs. Show less



The University of Western Australia

• Australia
• Higher Education
• 700 & Above Employee

• Research Fellow

  • Sep 2007 - Sep 2009

  i) 4D reconstruction of the iron deposit (Eastern Hamersley Basin, WA) ii) 4D architecture of the 2.9 Ga nickel deposit (Lake Johnston, WA); iii) Determination of continuity of greenstone belt under cover in Zimbabwe Craton. i) 4D reconstruction of the iron deposit (Eastern Hamersley Basin, WA) ii) 4D architecture of the 2.9 Ga nickel deposit (Lake Johnston, WA); iii) Determination of continuity of greenstone belt under cover in Zimbabwe Craton.



University of Orleans

• Chemical Manufacturing
• 1 - 100 Employee

• PhD student

  • Sep 2004 - Jun 2007

  The tectonic role and geodynamic significance of major discontinuities in the late to post-orogenic evolution are questioned in the Variscan belt. The Sillon Houiller Fault (SHF) is a major sub meridian discontinuity which pre-Stephanian kinematics and evolution remain poorly understood. In order to better understand the role of the SHF during the late Variscan evolution of the French Massif Central, a multidisciplinary study has been carried out on some of the massifs which are situated along the fault: petrology, geochronology, Anisotropy of Magnetic Susceptibility (AMS), gravity as well as interpretation of aeromagnetic survey. New geophysical, field and AMS data have been integrated into 2D and 3D, forward and inverse, geophysical and geological models, which highlight the geometry and the emplacement of syn-tectonic Namurian plutons. These results allow us to draw the following major conclusions. In Namurian time, the SHF may be related to magma emplacement, as for the Montmarault pluton in the north, or not, as for the Glénat, Omps and Boisset massifs in the south. Nevertheless, all the analyzed granitic plutons record a NW-SE stretching direction, perpendicular to the general strike of the SHF. From our structural and kinematics analysis, in Namurian time, if the SHF existed, it should behave as a NW-SE dilatant zone. Show less