Crustal architecture of a metallogenic belt and ophiolite belt: implications for mineral genesis and emplacement from 3-D electrical resistivity models (Bayankhongor area, Mongolia)
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 s...
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Dokumenttypen: | Artikel |
Medientypen: | Text |
Erscheinungsdatum: | 2021 |
Publikation in MIAMI: | 28.04.2023 |
Datum der letzten Änderung: | 28.04.2023 |
Angaben zur Ausgabe: | [Electronic ed.] |
Quelle: | Earth, Planets and Space 73 (2021), 82, 1-20 |
Schlagwörter: | Metallogenic belt; Ophiolite belt; Fault zone; Mineralization; Mineral emplacement; Electrical resistivity |
Fachgebiet (DDC): | 530: Physik |
Lizenz: | CC BY 4.0 |
Sprache: | English |
Förderung: | Finanziert über die DEAL-Vereinbarung mit Wiley 2019-2022. Förderer: Deutsche Forschungsgemeinschaft / Projektnummer: 431487296 Förderer: Swiss National Science Foundation / Projektnummer: 189177 |
Format: | PDF-Dokument |
URN: | urn:nbn:de:hbz:6-20059545824 |
Weitere Identifikatoren: | DOI: 10.17879/40059700662 |
Permalink: | https://nbn-resolving.de/urn:nbn:de:hbz:6-20059545824 |
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Onlinezugriff: | 10.1186_s40623-021-01400-9.pdf |
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 ( 1000 Ωm), low-resistivity (