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  • 1
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (95 Blatt = 32 MB) , Illustrationen, Diagramme, Karten
    Language: English
    Note: Zusammenfassung in deutscher und englischer Sprache
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  • 2
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    In:  [Poster] In: 81. Jahrestagung der Deutschen Geophysikalischen Gesellschaft (DGG), 01.03.-05.03.2021, Kiel (online) .
    Publication Date: 2021-07-12
    Description: Combined analysis of multiple geophysical methods is a key practice to reduce model uncertainties and improve geological interpretations. Various approaches to combine several data sets or physical models in joint inversion have different advantages and challenges. We present a comparison of two ways to integrate marine magnetotelluric (MT) with gravity data along the Namibian passive continental margin and also compare them to a single-method MT inversion. This study area offers an excellent setting, because multiple tectonic processes (e.g. rifting, magmatism, post-breakup sedimentation) lead to various lithological units with distinct physical properties (e.g. continental-, transitional-, and oceanic crust, fault systems or sedimentary depocenters). The two joint inversions are a cross-gradient coupled 3D inversion of marine magnetotelluric data with a fixed structural density model based on gravity modeling, and a joint inversion of the same MT data with satellite gravity data. Structural coupling with the blocky density model enforces harsh resistivity changes in an otherwise smooth model and helps reducing excessively smeared inversion artifacts. Although the edge-like features complicate direct model interpretation, they indicate alternative ways to fit the MT data, while simultaneously matching seismic observations integrated in the density cross-model. For the second approach, the large solution space of the satellite gravity data inversion limits the improvements through joint inversion compared to a single method MT inversion. The resulting joint inversion resistivity model differs only marginally from the single-method resistivity model, while the joint density model inherits some of the rather questionable resistivity model features. Our study demonstrates how joint inversion of multiple data aids model interpretation. The resulting resistivity models provide equally well-fitting alternatives to single-method evaluation, and additionally fit other geophysical method’s observations (i.e. gravity and seismic methods). The direct comparison of the impact of constraining MT inversion with either a fixed structural model or a coupled data inversion highlights how well the MT solution space may be confined. In our study, the fixed structural model constraint outperforms the joint MT-gravity data analysis.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 3
    Publication Date: 2020-11-23
    Description: Highlights • We report on marine 3D Magnetotelluric study on Walvis Ridge • Derived 3D electrical resistivity model shows a large scale resistive zone, which we link to crustal extension due to local uplift. It might indicate the location where the hot-spot impinged on the crust prior to rifting • Smaller scale resistive region is attributed to magma ascent during rifting • Rift basin is identified by low resistivity region The Namibian continental margin marks the starting point of the Tristan da Cunha hotspot trail, the Walvis Ridge. This section of the volcanic southwestern African margin is therefore ideal to study the interaction of hotspot volcanism and rifting, which occurred in the late Jurassic/early Cretaceous. Offshore magnetotelluric data image electromagnetically the landfall of Walvis Ridge. Two large-scale high resistivity anomalies in the 3-D resistivity model indicate old magmatic intrusions related to hot-spot volcanism and rifting. The large-scale resistivity anomalies correlate with seismically identified lower crustal high velocity anomalies attributed to magmatic underplating along 2-D offshore seismic profiles. One of the high resistivity anomalies (above 500 Ωm) has three arms of approximately 100 km width and 300 km to 400 km length at 120 degree angles in the lower crust. One of the arms stretches underneath Walvis Ridge. The shape is suggestive of crustal extension due to local uplift. It might indicate the location where the hot-spot impinged on the crust prior to rifting. A second, smaller anomaly of 50 km width underneath the continent ocean boundary may be attributed to magma ascent during rifting. We attribute a low resistivity anomaly east of the continent ocean boundary and south of Walvis Ridge to the presence of a rift basin that formed prior to the rifting.
    Type: Article , PeerReviewed
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  • 4
    Publication Date: 2021-01-20
    Description: SO277 OMAX served two scientific projects. The objectives of the first project, SMART, were to develop multi-disciplinary methodologies to detect, quantify, and model offshore groundwater reservoirs in regions dominated by carbonate geology such as the Mediterranean Sea. To this end we acquired controlled-source electromagnetic, seismic, hydroacoustic, geochemical, seafloor imagery data off Malta. Preliminary evaluation of the geophysical data show that there are resisitivity anomalies that may represent offshore freshwater aquifers. The absence of evidence for offshore springs means that these aquifers would be confined and that it will be difficult to use them in a sustainable manner. The objective of the second project, MAPACT-ETNA, is to monitor the flank of Etna volcano on Sicily which is slowly deforming seaward. Here, we deployed six seafloor geodesy stations and six ocean bottom seismometers for long-term observation (1-3 years). In addition, we mapped the seafloor off Mt. Etna and off the island of Stromboli to constrain the geological processes that control volcanic flank stability.
    Type: Report , NonPeerReviewed
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  • 5
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    In:  [Poster] In: 27. Schmucker-Weidelt-Kolloquium für Elektromagnetische Tiefenforschung (EMTF 2017), 25.-29.09.2017, Breklum, Germany .
    Publication Date: 2018-01-04
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 6
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    In:  [Poster] In: EM Induction Workshop 2016, 14.-20.08.2016, Chiang Mai, Thailand .
    Publication Date: 2018-01-29
    Description: We present a three-dimensional resistivity model derived from a large-scale magnetotelluric experiment offshore Namibia. To obtain the model we use the inversion code "mtinv" based on an integral equation approach (see Avdeev&Avdeeva, 2009, Avdeeva et al., 2012 and Moorkamp et al., 2010). The code allows positioning of MT sites at the sea-floor and inclusion of bathymetry. However, the bathymetry is approximated with a rectilinear mesh, which is not optimal as a large portion of the computationally feasible grid is used up by bathymetry, at the same time reducing the resolution of the upper region. Nevertheless, we observe a good correlation of the boundaries of large-scale resistive anomalies with seismically identified lower crustal high-velocity structures. This gives us confidence in the large-scale features of the resistivity model. Together with information from 2-D seismic profiles and on-shore geology the resistivity model provides valuable insight into the spatial distribution of increased magmatic activity.
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 7
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    In:  (Master thesis), Christian-Albrechts-Universität zu Kiel, Kiel, Germany, 87 pp
    Publication Date: 2018-01-04
    Description: The source of magmatic features along the Namibian continental margin, and therefore the processes which lead to the opening of the South Atlantic ocean, are still debated controversially. One big question is weather hotspot volcanism was fed by a deep reaching plume or by heterogeneities of the middle and upper mantle. In an attempt to gain a better understanding of the involved magmatic processes, a 3D inversion of magnetotelluric data with an integrated seismically constrained density model was conducted. Integration was accomplished by adding a cross-gradient constraint of the density model to the inversion, which enforces model resemblance at structural boundaries. The impact of this cross-gradient constraint with a preexisting density model is limited to this model's resolution, because the cross-gradient only works at structural boundaries within the constraint model. Its benefits include enhancing of resistivity structures in the inversion model. Additionally, the density constraint does not overprint resistivity structures which are not imaged by gravimetric methods (i.e. resistivity variations due to mineral composition). An observed high resistivity anomaly below the continental margin and Walvis Ridge coincides well with seismically observed high velocity underplating. This feature is interpreted to mark magmatic intrusions from a plume source, initiating continental breakup. The eastern termination of the high resistivity structure correlates with the onset of seaward dipping reflectors in seismic data. Therefore, it marks the transition from continental to oceanic regime (continent-ocean boundary). The theory of a plume source of the magmatic features is supported by the local planar extent of roughly estimated 70 000km² and the deep reaching form of the underplating. This form with three arms at a 120° spread is suggestive for the rift arms of a hot spot impingement into the crust. However, since the aforementioned amount of intrusive material is rather small for the impact of a road plume head, the preferred model includes a plume that stopped ascending in the mid-mantel. The underplated magmatic features would then be fed by smaller plumes or hotspot-like dikes rising from this deep mantle plume. A continental breakup solely driven by plate-forces is unlikely for the South Atlantic, as lithospheric thinning and subsequent magmatism would have resulted in a larger volcanic area due to mantle heterogeneities, than the observed local magmatic underplating.
    Keywords: Course of study: MSc Geophyscis
    Type: Thesis , NonPeerReviewed
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  • 8
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    In:  [Poster] In: EGU General Assembly 2020, 03.05.-08.05.2020, Vienna, Austria - Online .
    Publication Date: 2021-01-18
    Description: Geophysical inversion always faces the problem of ambiguity, where several earth models can describe the same data. To tackle this issue, additional information can be integrated by joint inversion of different data sets (Heincke et al., 2017; Moorkamp, 2017; Moorkamp et al., 2011), or by cooperative inversion through relating physical models derived from independent data (Bedrosian, 2007; Gallardo, 2004; Haber & Oldenburg, 1997; Lines et al., 1987; Paasche & Tronicke, 2007).Here we present our recent results of joint- and cooperative inversions along the Namibian passive continental margin and Walvis Ridge investigating break-up related magmatism. Jegen et al. (2016), presents a resistivity model derived from Magnetotelluric data acquired in 2011 (SAMPLE project). We reevaluate this data due to a previous rotation error, and implement three additional set ups, wherea)MT data inversion is constrained by a geological model derived from gravity modeling (Maystrenko et al., 2013)b)marine MT- and satellite gravity data are jointly inverted with a common objective functionc)a 2D velocity model (Fromm et al., 2017) is used as a structural constraint in 3D MT inversion
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 9
    Publication Date: 2018-09-07
    Type: Conference or Workshop Item , NonPeerReviewed
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  • 10
    Publication Date: 2023-02-09
    Description: 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 parameters. Particularly in complex geological scenarios, such as the rifted passive margin offshore Namibia, multi-parameter analysis and joint inversion are key techniques for comprehensive geological inferences. The models resulting from joint inversion enable the definition of specific parameter combinations, which can then be ascribed to geological units. Here we perform a user-unbiased clustering analysis of the parameters electrical resistivity and density from two models derived in a joint inversion along the Namibian passive margin. We link the resulting parameter combinations to break-up related lithology, and infer the history of margin formation. This analysis enables us to clearly differentiate two types of sediment cover. Namely, one of near-shore, thick, clastic sediments, and a second one of further offshore located, more biogenic, marine sediments. Furthermore, we clearly identify areas of interlayered massive, and weathered volcanic flows, which are usually only identified in reflection seismic studies as seaward dipping reflectors. Lastly, we find a distinct difference in the signature of the transitional crust south of- and along the supposed hot-spot track Walvis Ridge. We ascribe this contrast to an increase in magmatic activity above the volcanic centre along Walvis Ridge, and potentially a change in melt sources or depth of melting. This characterizes a rift-related southern complex, and a plume-driven Walvis Ridge regime. All of these observations demonstrate the importance of multi-parameter geophysical analysis for large-scale geological interpretations. Furthermore, our results may improve future joint inversions using direct parameter coupling, by providing a guideline for the complex passive margins parameter correlations.
    Type: Article , NonPeerReviewed
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