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1000 Titel
  • Crustal architecture of a metallogenic belt and ophiolite belt: implications for mineral genesis and emplacement from 3-D electrical resistivity models (Bayankhongor area, Mongolia)
1000 Autor/in
  1. Comeau, Matthew Joseph |
  2. Becken, Michael |
  3. Kuvshinov, Alexey V. |
  4. Demberel, Sodnomsambuu |
1000 Erscheinungsjahr 2021
1000 Publikationstyp
  1. Artikel |
1000 Online veröffentlicht
  • 2021-04-01
1000 Erschienen in
1000 Quellenangabe
  • 73(1):82
1000 Copyrightjahr
  • 2021
1000 Lizenz
1000 Verlagsversion
  • https://doi.org/10.1186/s40623-021-01400-9 |
  • https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8550322/ |
1000 Publikationsstatus
1000 Sprache der Publikation
1000 Abstract/Summary
  • Crustal architecture strongly influences the development and emplacement of mineral zones. In this study, we image the crustal structure beneath a metallogenic belt and its surroundings in the Bayankhongor area of central Mongolia. In this region, an ophiolite belt marks the location of an ancient suture zone, which is presently associated with a reactivated fault system. Nearby, metamorphic and volcanic belts host important mineralization zones and constitute a significant metallogenic belt that includes sources of copper and gold. However, the crustal structure of these features, and their relationships, are poorly studied. We analyze magnetotelluric data acquired across this region and generate three-dimensional electrical resistivity models of the crustal structure, which is found to be locally highly heterogeneous. Because the upper crust (< 25 km) is found to be generally highly resistive (> 1000 Ωm), low-resistivity (< 50 Ωm) features are conspicuous. Anomalous low-resistivity zones are congruent with the suture zone, and ophiolite belt, which is revealed to be a major crustal-scale feature. Furthermore, broadening low-resistivity zones located down-dip from the suture zone suggest that the narrow deformation zone observed at the surface transforms to a wide area in the deeper crust. Other low-resistivity anomalies are spatially associated with the surface expressions of known mineralization zones; thus, their links to deeper crustal structures are imaged. Considering the available evidence, we determine that, in both cases, the low resistivity can be explained by hydrothermal alteration along fossil fluid pathways. This illustrates the pivotal role that crustal fluids play in diverse geological processes, and highlights their inherent link in a unified system, which has implications for models of mineral genesis and emplacement. The results demonstrate that the crustal architecture-including the major crustal boundary-acts as a first-order control on the location of the metallogenic belt.!##!Supplementary information!#!The online version contains supplementary material available at 10.1186/s40623-021-01400-9.
1000 Sacherschließung
lokal Ophiolite belt
lokal 1. Geomagnetism
lokal Mineral emplacement
lokal Mineralization
lokal Electrical resistivity
lokal Fault zone
lokal Full Paper
lokal Metallogenic belt
1000 Liste der Beteiligten
  1. https://orcid.org/0000-0003-0807-7240|https://frl.publisso.de/adhoc/uri/QmVja2VuLCBNaWNoYWVs|https://frl.publisso.de/adhoc/uri/S3V2c2hpbm92LCBBbGV4ZXkgVi4=|https://frl.publisso.de/adhoc/uri/RGVtYmVyZWwsIFNvZG5vbXNhbWJ1dQ==
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1000 Erstellt am 2023-04-26T13:11:19.940+0200
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