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  • 1
    Monograph available for loan
    Monograph available for loan
    Aachen : Shaker Verl.
    Call number: M 02.0460
    Type of Medium: Monograph available for loan
    Pages: 170 S.
    ISBN: 3832202242
    Series Statement: Berichte aus der Geowissenschaft
    Classification:
    Regional Geology
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Monograph available for loan
    Monograph available for loan
    Call number: M 05.0121
    Type of Medium: Monograph available for loan
    Pages: 136 S. , graph. Darst.
    Note: Bonn, Univ., Diss., 1994
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
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    PANGAEA
    In:  Supplement to: Warsitzka, Michael; Kukowski, Nina; May, Franz (2019): The formation of forced Folds and wing-like sand intrusions driven by pore fluid overpressure: Implications from 2D experimental modeling. Journal of Geophysical Research: Solid Earth, https://doi.org/10.1029/2019JB018120
    Publication Date: 2023-01-13
    Description: Sand injections form by intrusion of overpressured, fluidized sand into surrounding low-permeable, fine-grained rocks. We conducted a series of scaled analog experiments to investigate the kinematic evolution of sand injections originating from an overpressured, tabular source layer associated with forced folding and propagation of fractures. The experiments were performed in the analog laboratory of the Institute of Geosciences (Friedrich Schiller University Jena) in the framework of the project "Mobilization of Unconsolidated Sediments Related to CO2 Storage". The layering of the analog materials consisted of non-cohesive and cohesive granulates to mimic a sand reservoir and its fine-grained overburden. To produce a fluid overpressure in the layered materials, air was injected from the base of the reservoir layer and additionally through a point-like needle valve penetrating into the reservoir layer. Pressure sensors recorded the air pressure at the base of the reservoir layer and in the needle valve. The experiments were monitored with a digital SLR camera and analyzed by the digital image correlation software DaVis 10.0 (LaVision GmbH) to calculate displacement and strain patterns in the analog materials. The data set presented here includes (1) original data: - Photos of the experimental evolution - Data of volumetric air flow rate and air pressure recorded during the experiments and (2) analyzed data: - Results of digital image correlation including edited photographs as well as data and plots of the displacement vector fields - Edited photos and a Python script for analyzing the vertical displacements of the experimental surface. Detailed descriptions of the experiments, method and results can be found in Warsitzka, et al. (2019) to which this data set is supplement.
    Keywords: Analog modeling; digital image correlation; File content; File format; File name; File size; pore fluid overpressure; sand injection; Uniform resource locator/link to file
    Type: Dataset
    Format: text/tab-separated-values, 20 data points
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  • 4
    Publication Date: 2024-04-20
    Description: Forced folding of a low-permeable, competent sediment layer in response to magmatic sill intrusion, remobilisation of fluidized sand or fluid overpressure in underlying porous reservoir formations can cause the formation of complex fracture networks. The opening modes and geometries of these fractures affect the bulk permeability of the cover layer and, thus, are crucial for understanding fluid flow processes in sedimentary basins. We carried out analog experiments in the laboratory of the Institute of Geosciences, Friedrich Schiller University Jena (project: Mobilization of Unconsolidated Sediments Related to CO2 Storage) to simulate the evolution of fracture networks during forced folding, its differences between a 2D and 3D modelling approach and its variability depending on the rheological stratification of the cover. To produce a fluid overpressure in the layered analog materials, air was injected from the base of the layering and additionally through a point-like needle valve penetrating into the lowermost layer with a stepwise increasing air flux (Q). Pressure sensors recorded the air pressure at the base of the reservoir layer and in the needle valve. The experiments were monitored with a digital SLR camera and analyzed by the digital image correlation software DaVis 10.0 (LaVision GmbH) to calculate displacement and strain patterns in the analog materials. Furthermore, a fracture analysis was performed for which we measured length and dips or strikes, respectively, in the side view of the 2D experiments and in top view in the 3D experiments. Based on these data, opening modes of the fractures were determined and statistical analyses were applied. The outcomes of these analyses are shown in rose diagram and histograms. The data set presented here includes: 1) Original data: -PhotosOriginal.zip: Photos of the experimental evolution -FractureData.zip: Measured lengths and dips (from side views of the 2D experiments) or strikes (from top view of the 3D experiments) of individual fracture segments -PneumaticData.zip: Data of volumetric air flow rate (Q) and air pressure (P) recorded during the experiments 2) Analyzed data: -DigitalImageCorrelation.zip: Results of digital image correlation including edited photographs as well as data and plots of the displacement vector fields -SurfaceDisplacement.zip: Edited photos and a Python script for analyzing the vertical displacements of the experimental surface. -RoseDiagrams.zip: Rose diagrams plotting the dips or strikes, respectively, of the fracture segments -Histograms.zip: Histogram showing the abundance of fracture segments along the vertical z-axis in the 2D experiments or along the horizontal x and y axes in the 3D experiments Detailed descriptions of the experiments, method and results can be found in Warsitzka, et al. (2022) to which this data set is supplement.
    Keywords: Analog modeling; Binary Object; Binary Object (File Size); Digital camera, Nikon D7000; digital image correlation; EXP; Experiment; failure mode; fluid overpressure; Forced folding; fracture analysis; IGWJena_Exp_2016; Jena, Germany; shear failure; tensile failure
    Type: Dataset
    Format: text/tab-separated-values, 7 data points
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  • 5
    Electronic Resource
    Electronic Resource
    Springer
    International journal of earth sciences 85 (1996), S. 782-799 
    ISSN: 1437-3262
    Keywords: Mineral water ; Tectonics Hydrodynamics ; Hydrothermal alteration ; Flow systems ; Rhenish Massif
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract Three major, interdependent processes control the genesis and distribution of mineral and thermal waters in the Rhenish Massif, Central Europe: (a) Magmatic processes in the upper mantle provide most of the CO2 to produce bicarbonate waters in shallow aquifers. (b) Extension of the brittle upper crust enables the ascent of sodium chloride waters. (c) Uplift and erosion shape the massif's relief, which determines the extent of flow systems and the distribution of thermal springs. The chemistry of mineral waters further depends on the aquifers' mineral composition. A comprehensive set of hydrological, chemical, tectonic and geophysical data on the Rhenish Massif has been compiled. It was used to classify the mineral waters and to map the spatial distribution of water properties. The composition of cuttings from several representative wells producing different water types shows that the hydrothermal alteration of the aquifer rocks consists mainly of kaolinization of chlorite and dissolution of feldspar. Numerical transport simulations favour two modes of groundwater flow: topography-driven flow and the pressure-driven ascent of basement brines along active faults. Thermal convection is less important.
    Type of Medium: Electronic Resource
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  • 6
    ISSN: 0016-7835
    Keywords: Key words Mineral water ; Tectonics ; Hydrodynamics ; Hydrothermal alteration ; Flow systems ; Rhenish Massif
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Notes: Abstract  Three major, interdependent processes control the genesis and distribution of mineral and thermal waters in the Rhenish Massif, Central Europe: (a) Magmatic processes in the upper mantle provide most of the CO2 to produce bicarbonate waters in shallow aquifers. (b) Extension of the brittle upper crust enables the ascent of sodium chloride waters. (c) Uplift and erosion shape the massif's relief, which determines the extent of flow systems and the distribution of thermal springs. The chemistry of mineral waters further depends on the aquifers' mineral composition. A comprehensive set of hydrological, chemical, tectonic and geophysical data on the Rhenish Massif has been compiled. It was used to classify the mineral waters and to map the spatial distribution of water properties. The composition of cuttings from several representative wells producing different water types shows that the hydrothermal alteration of the aquifer rocks consists mainly of kaolinization of chlorite and dissolution of feldspar. Numerical transport simulations favour two modes of groundwater flow: topography-driven flow and the pressure-driven ascent of basement brines along active faults. Thermal convection is less important.
    Type of Medium: Electronic Resource
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  • 7
    Publication Date: 2023-03-16
    Description: Ein aktuelles Verzeichnis und eine Karte der Verbreitung der Säuerlinge und Mofetten in der Vulkaneifel und der Südeifel werden vorgestellt. Die Problematik der Abgrenzung von Mineralwässern und Süßwässern wird diskutiert und Grenzwerte für charakteristische Inhaltsstoffe vorgeschlagen. Untersuchungen der Schüttungsmengen und der Gasführung der Mineralquellen bilden die Basis für eine Bilanz des CO2- Flusses im Untersuchungsgebiet. Zahlreiche in der geologischen Literatur beschriebene Quellen sind heute nicht mehr vorhanden, was vielfach auf menschliche Einwirkungen zurückgeführt werden kann. Der derzeitige vorgefundene Zustand der Quellen wird kurz skizziert. Damit liegt eine aktuelles, überprüftes Verzeichnis vor, das dem Geotopschutz verbliebener natürlicher Mineralquellen als Grundlage dienen kann.
    Description: Abstract: An up-to-date register and a map of the distribution of the carbonic mineral springs and mofettes (dry, cold CO2-emissions) in the Westeifel volcanic field and the Southern Eifel is presented. The distinction between mineralised and fresh ground waters is discussed and threshold concentrations for discriminating dissolved species are proposed. A balance of the CO2 flux of the volcanic field has been calculated from discharge and gas flux measurements. Many springs mentioned in older geological publications do not exist anymore. Several of them have been destroyed by man. The present conditions of the springs is briefly documented in the register. This list should be used as base for the protection of the remaining natural mineral springs.
    Description: research
    Keywords: ddc:553.73 ; Eifel ; Mineralwasser ; Quellen ; Mofetten
    Language: German
    Type: doc-type:article , publishedVersion
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  • 8
    Publication Date: 2016-11-01
    Print ISSN: 1430-483X
    Electronic ISSN: 1432-1165
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences
    Published by Springer
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  • 9
    Publication Date: 2016-02-16
    Print ISSN: 1430-483X
    Electronic ISSN: 1432-1165
    Topics: Energy, Environment Protection, Nuclear Power Engineering , Geosciences
    Published by Springer
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  • 10
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