| Formation of continental microplates through rift linkage: Numerical modeling and its application to the Flemish Cap and Sao Paulo Plateau D Neuharth, S Brune, A Glerum, C Heine, JK Welford Geochemistry, Geophysics, Geosystems 22 (4), e2020GC009615, 2021 | 49 | 2021 |
| Evolution of rift systems and their fault networks in response to surface processes D Neuharth, S Brune, T Wrona, A Glerum, J Braun, X Yuan Tectonics 41 (3), e2021TC007166, 2022 | 29 | 2022 |
| Controls on asymmetric rift dynamics: Numerical modeling of strain localization and fault evolution in the Kenya Rift MJEA Richter, S Brune, S Riedl, A Glerum, D Neuharth, MR Strecker Tectonics 40 (5), e2020TC006553, 2021 | 21 | 2021 |
| Flexural strike-slip basins D Neuharth, S Brune, A Glerum, CK Morley, X Yuan, J Braun Geology 50 (3), 361-365, 2022 | 12 | 2022 |
| Hindered trench migration due to slab steepening controls the formation of the Central Andes M Pons, SV Sobolev, S Liu, D Neuharth Journal of Geophysical Research: Solid Earth 127 (12), e2022JB025229, 2022 | 8 | 2022 |
| Temporal variations in plume flux: characterizing pulsations from tilted plume conduits in a rheologically complex mantle D Neuharth, E Mittelstaedt Geophysical Journal International 233 (1), 338-358, 2023 | 3 | 2023 |
| From orogeny to rifting: the role of inherited structures during the formation of the South China Sea K Li, S Brune, D Neuharth, G Mohn, A Glerum, Z Erdös EGU General Assembly Conference Abstracts, EGU-7518, 2023 | 1 | 2023 |
| Trench migration and slab buckling control the formation of the Central Andes M Pons, SV Sobolev, S Liu, D Neuharth EarthArXiv, 2022 | 1 | 2022 |
| 2D geodynamic subduction model of the Central Andes M Pons, SV Sobolev, S Liu, D Neuharth GFZ Data Service, 2022 | 1 | 2022 |
| Development of Williams Ridge (Kerguelen Plateau) and Broken Ridge: Tectonics, Hotspot Magmatism, Microcontinents, and Australias Extended Continental Shelf M Coffin, J Whittaker, N Daczko, J Halpin, G Bernardel, K Picard, ... AGU Fall Meeting Abstracts 2021, T45A-0190, 2021 | 1 | 2021 |
| Temporal variations in hotspot volcanic production caused by interactions between upwelling mantle plumes and phase transitions DJ Neuharth, EL Mittelstaedt AGU Fall Meeting Abstracts 2017, DI11A-0262, 2017 | 1 | 2017 |
| To rotate or to link? The connection between the red sea and Gulf of Aden rifts in central afar A Muluneh, S Brune, C Pagli, A La Rosa, D Keir, D Neuharth, G Corti Geophysical Research Letters 51 (12), e2024GL108732, 2024 | | 2024 |
| Influence of the fluid pressure ratio on accretionary wedge evolution over long timescales D Neuharth, W Behr, A Holt, J Ruh EGU24, 2024 | | 2024 |
| How do the Red Sea and Gulf of Aden rifts connect? A Muluneh, S Brune, C Pagli, A La Rosa, D Keir, D Neuharth, G Corti EGU24, 2024 | | 2024 |
| 3D interaction of tectonics with surface processes explains fault network evolution of the Dead Sea Fault S Brune, EL Heckenbach, AC Glerum, R Granot, Y Hamiel, SV Sobolev, ... EGU24, 2024 | | 2024 |
| The influence of eclogitization in subduction: enhanced slab pull versus subduction interface jamming ACM Gomes, DJ Neuharth, W Behr, A Holt AGU23, 2023 | | 2023 |
| Normal fault network evolution in 3D numerical models S Brune, T Wrona, D Neuharth, A Glerum, J Naliboff, E Heckenbach EGU General Assembly Conference Abstracts, EGU-11050, 2023 | | 2023 |
| Numerically modelling along-strike rheologic variations in 3D subduction zones D Neuharth, W Behr, A Holt EGU General Assembly Conference Abstracts, EGU-11688, 2023 | | 2023 |
| Life and Death of Normal Faults: Quantitative Analysis of Fault Network Evolution in 3D Rift Models S Brune, T Wrona, D Neuharth, A Glerum, J Naliboff EGU General Assembly Conference Abstracts, EGU22-6294, 2022 | | 2022 |
| 3D geodynamic evolution of strike-slip restraining and releasing bends modulated by surface processes: application to the Dead Sea Transform E Heckenbach, S Brune, A Glerum, D Neuharth EGU General Assembly Conference Abstracts, EGU22-5427, 2022 | | 2022 |
Dr. Anne GlerumPostdoc GFZ Potsdam, Germany在 uu.nl 的电子邮件经过验证
