Judith Sippel
YOU?
Author Swipe
View article: Deep thermal field and rheology in different plate tectonic settings
Deep thermal field and rheology in different plate tectonic settings Open
Continental rifting and breakup as well as plate convergence and collision create specific geophysical configurations with characteristic thermal fields which in turn lead to characteristic rheological settings. Three-dimensional data-inte…
View article: Upper mantle shear-wave velocity conversions to temperature and density: open-source V2RhoT_gibbs sheds light into challenges and possibilities
Upper mantle shear-wave velocity conversions to temperature and density: open-source V2RhoT_gibbs sheds light into challenges and possibilities Open
Variations of seismic wave speed, in particular shear-wave velocity (vs), are largely temperature controlled in the Earth’s mantle. Seismic tomography models thus provide us with insights into upper mantle temperature variations, the…
View article: Thermal state of La Palma (Canary Islands) from a data-integrative approach
Thermal state of La Palma (Canary Islands) from a data-integrative approach Open
The Canary Islands stand out as a prime region within Spanish territory with significant potential for harnessing high enthalpy geothermal resources due to their active volcanic activity. La Palma, one of the youngest islands in the archip…
View article: Geodynamic controls on the geothermal potential in the Upper Rhine Graben, France-Germany: a multi-scale numerical modelling approach
Geodynamic controls on the geothermal potential in the Upper Rhine Graben, France-Germany: a multi-scale numerical modelling approach Open
The Upper Rhine Graben (URG), situated along the border of France and Germany, is part of the intraplate European Cenozoic Rift System. The graben is widely recognized for its abundant geothermal resources, making it a key region for energ…
View article: Contributions of plate strength and dip geometry on the localization of deformation in Central Andes: a data-driven modelling approach
Contributions of plate strength and dip geometry on the localization of deformation in Central Andes: a data-driven modelling approach Open
The southern Central Andes (29°S-39°S) is a key area for understanding the interplay between the oceanic plate and the continental plate and its resulting surface expressions in a subduction zone.  In this area, the dip of t…
View article: Has the Hainan plume interacted with the oceanic lithosphere of the South China Sea?
Has the Hainan plume interacted with the oceanic lithosphere of the South China Sea? Open
Seismic, petrological, and geochemical studies confirm the existence of the Hainan plume in SE Asia, but whether the plume interacted with the oceanic lithosphere of the South China Sea (SCS) has been a subject of debate. To address this p…
View article: Crustal Density Model of the Sea of Marmara: Geophysical Data Integration and 3D Gravity Modelling
Crustal Density Model of the Sea of Marmara: Geophysical Data Integration and 3D Gravity Modelling Open
The Sea of Marmara, in Northwest Turkey, is a transition zone where the dextral North Anatolian Fault Zone (NAFZ) propagates westward from the Anatolian plate to the Aegean plate. The area is of interest in the context of seismic hazard in…
View article: Lithospheric Control on Asthenospheric Flow From the Iceland Plume: 3‐D Density Modeling of the Jan Mayen‐East Greenland Region, NE Atlantic
Lithospheric Control on Asthenospheric Flow From the Iceland Plume: 3‐D Density Modeling of the Jan Mayen‐East Greenland Region, NE Atlantic Open
The density structure of the oceanic lithosphere north of Iceland is key for understanding the effects of the Iceland plume on the greater Jan Mayen‐East Greenland Region. We obtain the 3‐D density structure of the sediments and the crust …
View article: The tectonic inventory of the greater Kenya Rift region investigated by 3D numerical models of plume-lithosphere interactions
The tectonic inventory of the greater Kenya Rift region investigated by 3D numerical models of plume-lithosphere interactions Open
High-resolution numerical simulations of thermo-mechanical processes are nowadays capable of tracing localized\ncrustal deformation as a response to the interaction of plume dynamics and far-field tectonic stresses affecting the lithospher…
View article: The effects of regional fluid flow on the deep thermal field - a case study from the Federal State of Hesse (Germany)
The effects of regional fluid flow on the deep thermal field - a case study from the Federal State of Hesse (Germany) Open
Geothermal energy utilization for electric power generation was planned in the Federal State of Hesse at two sites. The first one in the northern part of the Upper Rhine Graben (south Hesse) has been drilled in 2016 but flow rates and temp…
View article: Variability of the geothermal gradient across passive continental margins of the North and South Atlantic Ocean
Variability of the geothermal gradient across passive continental margins of the North and South Atlantic Ocean Open
Comprehension of the lithosphere-scale thermal field at passive continental margins is a key to unravel obscure processes of the plate tectonic cycle and to explore the subsurface resources. In this study, we investigate variations of the …
View article: Determining deep geothermal potentials based on integrated multi-scale datasets and models: case study of the Federal State of Hesse (Germany)
Determining deep geothermal potentials based on integrated multi-scale datasets and models: case study of the Federal State of Hesse (Germany) Open
For the Federal State of Hesse so far no regional assessment of petrothermal or medium deep geothermal resources for direct heat use and underground thermal energy storage (UTES) are available. The project “Hessen 3D 2.0” aims to bridge th…
View article: Density structure and rheology of northern Argentina: from the Central Andes to the foreland basin
Density structure and rheology of northern Argentina: from the Central Andes to the foreland basin Open
The Central Andes along with their related basins constitute a heterogeneous and complex system. Its present state results from the interaction of the recent Andean orogeny with inherited structures of the lithosphere. Several studies have…
View article: Variability of the geothermal gradient across two differently aged magma-rich continental rifted margins of the Atlantic Ocean
Variability of the geothermal gradient across two differently aged magma-rich continental rifted margins of the Atlantic Ocean Open
The aim of this study is to investigate the shallow thermal field differences for two differently aged passive continental margins by analyzing regional variations in geothermal gradient and exploring the controlling factors for these vari…
View article: Variability of the geothermal gradient across two differently aged magma-rich continental rifted margins of the Atlantic Ocean: the Southwest African and the Norwegian margins
Variability of the geothermal gradient across two differently aged magma-rich continental rifted margins of the Atlantic Ocean: the Southwest African and the Norwegian margins Open
The aim of this study is to investigate the shallow thermal field differences for two differently aged passive continental margins by analyzing regional variations in geothermal gradient and exploring the controlling factors for these vari…
View article: Crustal Structure of the Andean Foreland in Northern Argentina: Results From Data‐Integrative Three‐Dimensional Density Modeling
Crustal Structure of the Andean Foreland in Northern Argentina: Results From Data‐Integrative Three‐Dimensional Density Modeling Open
Previous thermomechanical modeling studies indicated that variations in the temperature and strength of the crystalline crust might be responsible for the juxtaposition of domains with thin‐skinned and thick‐skinned crustal deformation alo…
View article: From 3D gravity to coupled fluid and heat transport modelling - a case study from the Upper Rhine Graben
From 3D gravity to coupled fluid and heat transport modelling - a case study from the Upper Rhine Graben Open
Numerical models that predict and help to understand subsurface hydrothermal conditions are key to reduce the risk of drilling non-productive geothermal wells. Such simulations of coupled fluid and heat transport need a reliable 3D structu…
View article: Overcoming Spatial Scales in Geothermal Modelling for Urban Areas
Overcoming Spatial Scales in Geothermal Modelling for Urban Areas Open
A major component in the transition from fossil to renewable energy is the demand for district heating where geothermal energy can be a substantial option. We present results on the controlling factors for the deep thermal field below a la…
View article: Variability of geothermal gradient across two differently aged continental volcanic passive margins: The Southwest African and the Norwegian margins
Variability of geothermal gradient across two differently aged continental volcanic passive margins: The Southwest African and the Norwegian margins Open
The aim of this study is to investigate the shallow thermal field differences for two differently aged passive continental margins by analyzing regional variations in geothermal gradient and exploring the controlling factors for these vari…
View article: Mechanisms of crustal shortening in the foreland of the central Andes, Argentina: insights from data-driven three-dimensional gravity, thermal and rheological modelling
Mechanisms of crustal shortening in the foreland of the central Andes, Argentina: insights from data-driven three-dimensional gravity, thermal and rheological modelling Open
Thin- and thick-skinned deformation styles in the foreland of the central Andes are the result of ongoing crustal shortening since the early Neogene. The mechanisms proposed for these different styles range from variations in subduction an…
View article: The Kenya rift revisited: insights into lithospheric strength through data-driven 3-D gravity and thermal modelling
The Kenya rift revisited: insights into lithospheric strength through data-driven 3-D gravity and thermal modelling Open
We present three-dimensional (3-D) models that describe the present-day thermal and rheological state of the lithosphere of the greater Kenya rift region aiming at a better understanding of the rift evolution, with a particular focus on pl…
View article: The thermal field of the Upper Rhine Graben – Temperature predictions based on a 3D model
The thermal field of the Upper Rhine Graben – Temperature predictions based on a 3D model Open
The Upper Rhine Graben (URG) is one of the regions in Germany with promising potentials for deep geothermal energy production. As part of the EU - funded project “IMAGE” (Integrated Methods for Advanced Geothermal Exploration), we aim to u…
View article: The Kenya Rift revisited: insights into lithospheric strength through data-driven 3D gravity and thermal modelling
The Kenya Rift revisited: insights into lithospheric strength through data-driven 3D gravity and thermal modelling Open
We present 3D models that describe the present-day thermal and rheological state of the lithosphere of the greater Kenya Rift region aiming at a better understanding of the rift evolution, with a particular focus on plume-lithosphere inter…