Published December 17, 2024
| Version v1
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Polycyclic Andean-type orogenic evolution of the Dunhuang block in NW China: A result of Paleozoic reconfiguration of oceanic subduction systems
Authors/Creators
- 1. Institute of Geological Sciences, Polish Academy of Sciences
- 2. Université de Strasbourg, CNRS, ITES UMR 7063
- 3. Centre of Lithospheric Research, Czech Geological Survey
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4.
Guangzhou Institute of Geochemistry
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5.
Polish Academy of Sciences
Contributors
- 1. Institute of Geological Sciences, Polish Academy of Sciences
- 2. Université de Strasbourg, CNRS, ITES UMR 7063
- 3. Centre of Lithospheric Research, Czech Geological Survey
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4.
Guangzhou Institute of Geochemistry
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5.
Polish Academy of Sciences
Description
In this contribution we use structural, P–T and geochronological data of metamorphic rocks to characterize the Paleozoic tectono-thermal evolution of the Dunhuang block in NW China.
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Soldner_2025_Polycyclic Andean-type orogenic evolution of the Dunhuang block in NW China.pdf
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(44.1 MB)
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Additional details
Identifiers
Funding
- European Commission
- POLONEZ BIS - Postdoctoral Fellowships in Poland to Boost International Mobility and Skills Training 945339
- National Natural Science Foundation of China
- 42372240
- National Natural Science Foundation of China
- 42372225
- Chinese Academy of Sciences
- 132744KYSB20190039
- Czech Science Foundation
- 19-27682×
Dates
- Accepted
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2024-11-05