Articles | Volume 11, issue 1
https://doi.org/10.5194/se-11-199-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/se-11-199-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Dating tectonic activity in the Lepontine Dome and Rhone-Simplon Fault regions through hydrothermal monazite-(Ce)
Christian A. Bergemann
CORRESPONDING AUTHOR
Natural History Museum of Geneva, Geneva, Switzerland
Department of Earth Sciences, University of Geneva, Geneva, Switzerland
currently at: Institute of Earth Sciences, Heidelberg University, Heidelberg, Germany
Edwin Gnos
Natural History Museum of Geneva, Geneva, Switzerland
Alfons Berger
Institute of Geological Sciences, University of Bern, Bern, Switzerland
Emilie Janots
ISTerre, University of Grenoble, Grenoble, France
Martin J. Whitehouse
Swedish Museum of Natural History, Stockholm, Sweden
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Cited
14 citations as recorded by crossref.
- 独居石成因矿物学特征及其对U-Th-Pb年龄解释的制约 X. Liang et al. https://doi.org/10.3799/dqkx.2021.157
- Discovery and Implications of a Nanoscale Rare Earth Mineral in a Hyperaccumulator Plant L. He et al. https://doi.org/10.1021/acs.est.5c09617
- P–T-t conditions of successive deformation stages during exhumation of orogenically thickened crust; a case study from the Aar Massif, Central Alps, Switzerland E. Gnos et al. https://doi.org/10.1186/s00015-025-00484-9
- Petrogenesis of the Chamuhan Intrusion in the Southern Great Xing’an Range: Constraints from Zircon U-Pb Dating and Petrogeochemistry Y. Song et al. https://doi.org/10.3390/min15101085
- Constraining kinematic and temporal evolution of a normal-sense shear zone: Insights into the Simplon Shear Zone (Western Alps) C. Montemagni & S. Zanchetta https://doi.org/10.1016/j.jsg.2022.104557
- Bridging the Gap between Long–Term Orogenic Evolution (>10 Ma Scale) and Geomorphological Processes That Shape the Western Alps: Insights from Combined Dating Approaches Y. Rolland et al. https://doi.org/10.3390/geosciences12110393
- Episodes of fissure formation in the Alps: connecting quartz fluid inclusion, fissure monazite age, and fissure orientation data E. Gnos et al. https://doi.org/10.1186/s00015-021-00391-9
- Ion microprobe dating of fissure monazite in the Western Alps: insights from the Argentera Massif and the Piemontais and Briançonnais Zones E. Ricchi et al. https://doi.org/10.1186/s00015-020-00365-3
- Variations in the P‐T‐t of Deformation in a Crustal‐Scale Shear Zone in Metagranite T. Cawood & J. Platt https://doi.org/10.1029/2020GC009384
- Genetic study of the Shuangwang gold deposit in the Western Qinling, China: Constraints from monazite dating, S isotope, and Ca isotope compositions C. Binghan et al. https://doi.org/10.1016/j.oregeorev.2026.107143
- Cenozoic deformation in the Tauern Window (Eastern Alps) constrained by in situ Th-Pb dating of fissure monazite E. Ricchi et al. https://doi.org/10.5194/se-11-437-2020
- Extensional reactivation of the Penninic frontal thrust 3 Myr ago as evidenced by U–Pb dating on calcite in fault zone cataclasite A. Bilau et al. https://doi.org/10.5194/se-12-237-2021
- Reactive and resilient: the contrasting behaviour of monazite and titanite during deformation (the Forno-Rosarolo shear zone; Ivrea-Verbano Zone) A. Langone et al. https://doi.org/10.1017/S0016756825100022
- Analysis of the Mechanism of Ground Fissures in the Nairobi–Malaba Railway Rift Valley Area in Kenya B. Hao et al. https://doi.org/10.3389/feart.2022.916753
14 citations as recorded by crossref.
- 独居石成因矿物学特征及其对U-Th-Pb年龄解释的制约 X. Liang et al. https://doi.org/10.3799/dqkx.2021.157
- Discovery and Implications of a Nanoscale Rare Earth Mineral in a Hyperaccumulator Plant L. He et al. https://doi.org/10.1021/acs.est.5c09617
- P–T-t conditions of successive deformation stages during exhumation of orogenically thickened crust; a case study from the Aar Massif, Central Alps, Switzerland E. Gnos et al. https://doi.org/10.1186/s00015-025-00484-9
- Petrogenesis of the Chamuhan Intrusion in the Southern Great Xing’an Range: Constraints from Zircon U-Pb Dating and Petrogeochemistry Y. Song et al. https://doi.org/10.3390/min15101085
- Constraining kinematic and temporal evolution of a normal-sense shear zone: Insights into the Simplon Shear Zone (Western Alps) C. Montemagni & S. Zanchetta https://doi.org/10.1016/j.jsg.2022.104557
- Bridging the Gap between Long–Term Orogenic Evolution (>10 Ma Scale) and Geomorphological Processes That Shape the Western Alps: Insights from Combined Dating Approaches Y. Rolland et al. https://doi.org/10.3390/geosciences12110393
- Episodes of fissure formation in the Alps: connecting quartz fluid inclusion, fissure monazite age, and fissure orientation data E. Gnos et al. https://doi.org/10.1186/s00015-021-00391-9
- Ion microprobe dating of fissure monazite in the Western Alps: insights from the Argentera Massif and the Piemontais and Briançonnais Zones E. Ricchi et al. https://doi.org/10.1186/s00015-020-00365-3
- Variations in the P‐T‐t of Deformation in a Crustal‐Scale Shear Zone in Metagranite T. Cawood & J. Platt https://doi.org/10.1029/2020GC009384
- Genetic study of the Shuangwang gold deposit in the Western Qinling, China: Constraints from monazite dating, S isotope, and Ca isotope compositions C. Binghan et al. https://doi.org/10.1016/j.oregeorev.2026.107143
- Cenozoic deformation in the Tauern Window (Eastern Alps) constrained by in situ Th-Pb dating of fissure monazite E. Ricchi et al. https://doi.org/10.5194/se-11-437-2020
- Extensional reactivation of the Penninic frontal thrust 3 Myr ago as evidenced by U–Pb dating on calcite in fault zone cataclasite A. Bilau et al. https://doi.org/10.5194/se-12-237-2021
- Reactive and resilient: the contrasting behaviour of monazite and titanite during deformation (the Forno-Rosarolo shear zone; Ivrea-Verbano Zone) A. Langone et al. https://doi.org/10.1017/S0016756825100022
- Analysis of the Mechanism of Ground Fissures in the Nairobi–Malaba Railway Rift Valley Area in Kenya B. Hao et al. https://doi.org/10.3389/feart.2022.916753
Saved (final revised paper)
Latest update: 17 Jun 2026
Short summary
Metamorphic domes are areas in a mountain chain that were unburied and where deeper parts of the crust rose to the surface. The Lepontine Dome in the Swiss and Italian Alps is such a place, and it is additionally bordered on two sides by shear zones where crustal blocks moved past each other. To determine when these tectonic movements happened, we measured the ages of monazite crystals that form in fluid-filled pockets inside the rocks during these movements of exhumation and deformation.
Metamorphic domes are areas in a mountain chain that were unburied and where deeper parts of the...