Basin inversion as a driver of fluid flow and Pb-Zn mineralization in the Paleoproterozoic-earliest Mesoproterozoic Mount Isa mineral province: evidence from deep seismic reflection profiling and gravity modelling  


Authors / CoAuthors

Gibson, G.M. | Meixner, A.J. | Hutton, L.J. | Holzschuh, J.

Abstract

Abstract submitted to the 35th International Geological Congress, 27 August - 4 September 2016 Cape Town, South Africa. Deep seismic reflection profiling, combined with forward modelling of gravity data, lend strong support to the idea that the Paleo- to Mesoproterozoic Mount Isa mineral province comprises three vertically stacked and partially inverted sedimentary basins preserving a record of intracontinental rifting followed by passive margin formation.

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nonGeographicDataset

eCat Id

90062

Contact for the resource

  Custodian

RD  

  Owner

Australian National University  

  Custodian

Australian National University  
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  Point of contact

Commonwealth of Australia (Geoscience Australia)  
Cnr Jerrabomberra Ave and Hindmarsh Dr GPO Box 378
Canberra
ACT
2601
Australia

Keywords

  • External PublicationAbstract
  • QLD
Australian and New Zealand Standard Research Classification (ANZSRC)
  • Earth Sciences
  • Published_Internal

Publication Date

2016-01-01T00:00:00

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Australian Government Security ClassificationSystem    

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Creative Commons Attribution-NonCommercial 4.0 International Licence    

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geoscientificInformation

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This short abstract is an application for an oral presentation by George Gibson at the 35th International Geological Congress, 27 August - 4 September 2016 Cape Town, South Africa. It is based on a previoius paper;Gibson et al, 2015, Basin architecture and evolution in the Mount Isa mineral province, northern Australia: Constraints from deep seismic reflection profiling and implications for ore genesis, Ore Geology Reviews, in Press and available online, Feb 2016, http://www.sciencedirect.com/science/article/pii/S0169136815002036

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