Zobrazeno 1 - 10
of 59
pro vyhledávání: '"Max Moorkamp"'
Publikováno v:
Frontiers in Earth Science, Vol 11 (2023)
Density perturbations in the subsurface are the main driver of mantle convection and can contribute to lithospheric deformation. However, in many places the density structure in the subsurface is poorly constrained. Most geodynamic models rely on sim
Externí odkaz:
https://doaj.org/article/d77af725eea54255a6f4a16f80451cb6
Publikováno v:
Geophysical Journal International. 232:162-175
SUMMARY By combining gravity and magnetic data in a joint inversion approach, 3-D information on the crustal structure of Wilkes Land, East Antarctica, is obtained and possible geological features become evident. Both data sets are combined through a
Autor:
Max Moorkamp
The tectonic history of southern Africa includes Archean craton formation, multiple episodes of subduction and rifting and some of the world's most significant magmatic events. Lithospheric models based on seismological and magnetotelluric data show
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::eac9872d5335bb8740ded23f1aec34c6
https://doi.org/10.5194/egusphere-egu23-6068
https://doi.org/10.5194/egusphere-egu23-6068
Autor:
Maximilian Lowe, Tom Jordan, Max Moorkamp, Jörg Ebbing, Antonia Ruppel, Nikola Koglin, Chris Green, Mareen Lösing, Robert Larter
The Wilkes Subglacial Basin hosts potentially the largest unstable sector of the East Antarctica Ice Sheet due to the depth of the ice bed below sea level. Ice covering such basins poses a potentially high, but poorly constrained risk for future sea-
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::4b000703f098f2d0cfd9f6d8ff8edcd7
https://doi.org/10.5194/egusphere-egu23-368
https://doi.org/10.5194/egusphere-egu23-368
Autor:
Max Moorkamp
Geophysical methods such as seismology, magnetotellurics and gravity are key to reconstructing the structure of the upper mantle and inferring its composition. However, the relationship between composition and geophysical parameters, e.g. seismic vel
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::5b9a10d204e2456c9eb7d6dcaf9fc1f4
https://doi.org/10.5194/egusphere-egu23-7037
https://doi.org/10.5194/egusphere-egu23-7037
Greenland’s tectonic history is complex, and the resulting lithospheric structure is, although extensively studied, not well constrained. Most models agree regarding the location of the North Atlantic Craton in South Greenland, and the most recent
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8f34bfd325c427b4d5d2fee94ff8c533
https://doi.org/10.5194/egusphere-egu23-12192
https://doi.org/10.5194/egusphere-egu23-12192
Autor:
Graham Hill, Max Moorkamp, Yann Avram, Colin Hogg, Kati Mateschke, Sofia Gahr, Adam Schultz, Esteban Bowles-Martinez, Jared Peacock, Gokhan Karcioglu, Chaojian Chen, Corrado Cimarelli, Luca Carrichi, Yasuo Ogawa
Detection of geophysical signatures associated with a geologic event, such as a volcanic eruption, is key to understanding the underlying physical processes and making an accurate hazard assessment. Magma reservoirs are the main repositories for erup
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_________::8ddddfc22c348370dd5300cbe4a68587
https://doi.org/10.5194/egusphere-egu23-2969
https://doi.org/10.5194/egusphere-egu23-2969
Publikováno v:
eISSN
When interpreting geophysical models, we need to establish a link between the models' physical parameters and geological units. To define these connections, it is crucial to consider and compare geophysical models with multiple, independent parameter
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::8acd69be5e6cfeade2dc089b640152b7
https://egusphere.copernicus.org/preprints/2022/egusphere-2022-708/
https://egusphere.copernicus.org/preprints/2022/egusphere-2022-708/
Density perturbations in the subsurface are the main driver of mantle convection and can contribute to lithospheric deformation. However, in many places the density structure in the subsurface is poorly constrained. Most geodynamic models rely on sim
Externí odkaz:
https://explore.openaire.eu/search/publication?articleId=doi_dedup___::61952f6561640e4c2a0ddce8144ae158
https://hdl.handle.net/10919/114171
https://hdl.handle.net/10919/114171
Autor:
Scott R. Miller, Emilio L. Pueyo, Juliane Huebert, Ayush Kumar, Elisabet Beamud, Max Moorkamp, Nia Schamuells, Douwe J.J. van Hinsbergen, Ana Ruiz-Constán, Lisa Tauxe, C. Ayala, Shelby A Jones, Dibyendu Sur
Publikováno v:
Digital.CSIC. Repositorio Institucional del CSIC
instname
instname
This article is composed of three independent commentaries about the state of Integrated, Coordinated, Open, Networked (ICON) principles (Goldman et al., 2021, https://doi.org/10.1002/essoar.10508554.1) in the Geomagnetism, Paleomagnetism, and Electr