Dear Colleagues

 

The talk mentioned below may be of interest to some of you. 

 

Regards/Ken

 






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Our next TGDG event is scheduled in one week's time! We will be live 
broadcasting this talk. TGDG recommends using Google Chrome to run the virtual 
meeting.

 


 <https://www.tgdg.net/event-4146073> The PACIFIC project: Developing passive 
seismic techniques for environmentally friendly and cost-efficient mineral 
exploration


When: 02 Feb 2021 4:00 PM, EST
Live Online Broadcast:


Register here <https://attendee.gotowebinar.com/register/1642482768002248207> 

 

EVENT DETAILS:

Dr. Charles D. Beard, Postdoctoral Researcher, Sisprobe SAS and Universite 
Grenoble Alpes

Speaker Bio:

Charlie is a postdoc at Sisprobe <http://sisprobe.com/>  and the Université 
Grenoble Alpes <https://www.isterre.fr/>  with PACIFIC 
<https://www.pacific-h2020.eu/> , an EU project that develops passive seismic 
techniques for environmentally friendly and cost-efficient mineral exploration. 
Previously he worked at the British Geological Survey 
<https://www.bgs.ac.uk/research/minerals/oreDepositsAndCommodities.html> , 
Edinburgh with HiTech AlkCarb <http://carbonatites.eu/> , an EU project that 
investigated 'HiTech' raw materials (REE + HFSE) associated with alkaline rocks 
and carbonatites. He did his PhD at McGill University 
<https://www.mcgill.ca/eps/>  with a thesis on mineral-melt partitioning in 
alkaline magmatic systems 
<https://www.researchgate.net/publication/324601962_Interrogating_minerals_Deciphering_magmatic_REE_enrichment_processes_with_pyroxene_and_biotite>
 , in collaboration with GFZ Potsdam 
<https://www.gfz-potsdam.de/en/section/chemistry-and-physics-of-earth-materials/overview/>
 , Germany. He did his Masters with the Pacific Centre for Isotopic and 
Geochemical Research <http://pcigr.eos.ubc.ca/>  at UBC Vancouver 
<https://www.eoas.ubc.ca/> , and associated Arctic field mapping with the 
Geological Survey of Canada <http://www.largeigneousprovinces.org/18apr> . His 
undergraduate degree is from the University of Bristol 
<http://www.bristol.ac.uk/earthsciences/> .

Charlie’s research combines experiments, natural samples and numerical 
modelling to investigate magmatic processes, the evolution of the crust and the 
mantle, and the mineralisation of raw materials critical for renewable energy 
infrastructure. Recently he have become interested in how mineralogy, 
geochemistry and petrology can improve 3D geophysical models and ultimately 
streamline exploration efforts. This is will be the focus of his presentation 
to the TGDG.

Talk Abstract:

In the PACIFIC project we use two case studies to develop passive seismic 
techniques for application in mineral exploration: The Marathon PGE-Cu deposit 
in Ontario, Canada and the Kallak Fe deposits in Sweden. Passive seismic 
techniques are environmentally friendly and typically cost an order of 
magnitude less than active seismic surveys. Due to their sensitivity to 
contrasts in elastic properties, they are best applied to map sedimentary cover 
sequences and large-scale intrusive or fault structures that focus 
mineralisation. In special cases, such as with iron or manganese bodies, the 
mineralisation can be directly imaged.

Drillhole-constrained geological models at test sites allow us to determine (1) 
which geological features and resolved in our 3D seismic models and (2) develop 
data processing workflows that minimise the generation of artefacts. At the 
Marathon deposit most drilling extends ~ 400 m from surface. Our ambient noise 
surface wave tomography models image the footwall contact of the Coldwell 
complex, a structure that controls the location of PGE-Cu mineralisation at 
Marathon, and extend to a depth ~ 2 km from surface. There is, however, little 
to no contrast in seismic properties between mineralised and unmineralised 
gabbros at Marathon. At Kallak, a preliminary survey is used to image strongly 
deformed banded iron formation deposits hosted by gneisses. While there are 
limitations to the coverage provided by this preliminary survey, high velocity 
features in the 3D tomographic model correspond to drillhole-defined iron 
mineralisations, and similar high velocity features are imaged along strike. 
The strengths and limitations of passive seismic techniques are discussed, and 
directions of research are presented that aim to improve imaging of geological 
features at the prospect scale.

Live Online Broadcast:


Register/Log-In <https://attendee.gotowebinar.com/register/1642482768002248207> 
 

 

Please register/log-in for this online broadcast using the link above. TGDG 
members will also be able to view this presentation at a later date by visiting 
our member's only Talk Recordings 
<https://www.tgdg.net/members-only-talk-recodings>  page.

Membership:

Thank you for your continued support. If you haven't had a chance to renew, 
visit our membership page <https://www.tgdg.net/membership>  for a seamless 
transition to this year's exciting line-up.

Best regards,
 <https://www.tgdg.net/> Toronto Geological Discussion Group

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