Utilisation of probabilistic magnetotelluric modelling to constrain magnetic data inversion: proof-of-concept and field application

被引:5
|
作者
Giraud, Jeremie [1 ,2 ,3 ]
Seille, Hoel [4 ,5 ]
Lindsay, Mark D. [1 ,5 ,6 ]
Visser, Gerhard [5 ,7 ]
Ogarko, Vitaliy [1 ,2 ]
Jessell, Mark W. [1 ,2 ]
机构
[1] Univ Western Australia, Ctr Explorat Targeting, Sch Earth Sci, 35 Stirling Highway, Crawley, Australia
[2] Univ Western Australia, Mineral Explorat Cooperat Res Ctr, Sch Earth Sci, 35 Stirling Highway, Crawley, Australia
[3] Univ Lorraine, RING, GeoRessources, 2 Rue Doyen Marcel Roubault, Vandoeuvre Les Nancy, France
[4] Australian Resources Res Ctr, CSIRO Deep Earth Imaging Future Sci Platform, Kensington, NSW, Australia
[5] Australian Resources Res Ctr, CSIRO Mineral Resources, Kensington, NSW, Australia
[6] ARC Ind Transformat Training Ctr Data Analyt Reso, Sydney, NSW, Australia
[7] Univ Lorraine, GeoRessources, RING, 2 Rue Doyen Marcel Roubault, Vandoeuvre Les Nancy, France
关键词
MONTE-CARLO-SIMULATION; JOINT INVERSION; GEOPHYSICAL INVERSION; CLONCURRY DISTRICT; GEOLOGICAL MODELS; CRUSTAL STRUCTURE; 3D INVERSION; GRAVITY; UNCERTAINTY; INTEGRATION;
D O I
10.5194/se-14-43-2023
中图分类号
P3 [地球物理学]; P59 [地球化学];
学科分类号
0708 ; 070902 ;
摘要
We propose, test and apply a methodology integrating 1D magnetotelluric (MT) and magnetic data inversion, with a focus on the characterisation of the cover-basement interface. It consists of a cooperative inversion workflow relying on standalone inversion codes. Probabilistic information about the presence of rock units is derived from MT and passed on to magnetic inversion through constraints combining structural constraints with petrophysical prior information. First, we perform the 1D probabilistic inversion of MT data for all sites and recover the respective probabilities of observing the cover-basement interface, which we interpolate to the rest of the study area. We then calculate the probabilities of observing the different rock units and partition the model into domains defined by combinations of rock units with non-zero probabilities. Third, we combine these domains with petrophysical information to apply spatially varying, disjoint interval bound constraints (DIBC) to least-squares magnetic data inversion using the alternating direction method of multipliers (or ADMM). We demonstrate the proof-of-concept using a realistic synthetic model reproducing features from the Mansfield area (Victoria, Australia) using a series of uncertainty indicators. We then apply the workflow to field data from the prospective mining region of Cloncurry (Queensland, Australia). Results indicate that our integration methodology efficiently leverages the complementarity between separate MT and magnetic data modelling approaches and can improve our capability to image the cover-basement interface. In the field application case, our findings also suggest that the proposed workflow may be useful to refine existing geological interpretations and to infer lateral variations within the basement.
引用
收藏
页码:43 / 68
页数:26
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