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  • 1
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Inc
    Journal of metamorphic geology 19 (2001), S. 0 
    ISSN: 1525-1314
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Antitaxial non-deforming strain fringes from Lourdes, France, show complex quartz, calcite and chlorite fibre patterns that grew around pyrite in a slate during non-coaxial progressive deformation. Development of these fringes was modelled using a computer program ‘Fringe Growth 2.0’ which can simulate incremental growth of crystal fibres around core-objects of variable shape. It uses object-centre paths as input, which are obtained from fibre patterns in thin section. The numerical experiments produced fibre patterns that show complex intergrowth of displacement-controlled, face-controlled and intermediate fibres similar to those in the natural examples. The direction of displacement-controlled growth is only dependent on the relative movement between core-object and fringe, so that core-object rotation with respect to the fringe influences the fibre patterns and produces characteristic asymmetric fibre curvature. Object-centre paths should be used for kinematic analysis of strain fringes instead of single fibres since these paths represent the fringe as a whole. The length along the path can be interpreted in terms of finite strain and path curvature in terms of rigid body rotation of fringes with respect to an external reference frame.
    Type of Medium: Electronic Resource
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  • 2
    Electronic Resource
    Electronic Resource
    Springer
    Archives of gynecology and obstetrics 204 (1967), S. 59-67 
    ISSN: 1432-0711
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Zusammenfassung 1. Entsprechend der HypotheseLiebermans eines Zusammenhanges zwischen hyalinen Membranen der Neugeborenenlungen und einer Störung des fibrinolytischen Potentials wurden Neugeborenenlungen, Placentagewebe sowie Fruchtwasser nach der Plattenmethode vonAstrup-Albrechtsen untersucht. 2. Die vonLieberman angegebenen Ergebnisse ließen sich nicht reproduzieren. Nach unseren experimentellen Befunden dürfen hyaline Membranen nicht auf ein Faktorendefizit des fibrinolytischen Potentials des Lungengewebes zurückgeführt werden. 3. In Placenta und Fruchtwasser wurden Inhibitoren gegen Profibrinolysin-Aktivatoren und Fibrinolysin nachgewiesen. 4. Die lokale Bindung und Wirkung der Gewebsinhibitoren macht eine Intervention im fibrinolytischen Potential des Lungengewebes unwahrscheinlich; selbst bei möglichem Abstrom und Aspiration erscheint eine Beeinträchtigung des fibrinolytischen Potentials des Lungengewebes aus quantitativen Gründen nicht annehmbar.
    Type of Medium: Electronic Resource
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  • 3
    Electronic Resource
    Electronic Resource
    Springer
    Archives of dermatological research 218 (1964), S. 323-338 
    ISSN: 1432-069X
    Source: Springer Online Journal Archives 1860-2000
    Topics: Medicine
    Notes: Zusammenfassung In einer ausführlichen Darstellung werden die eigenen biochemischen Untersuchungen am menschlichen Spermaplasma zur Bestimmung von Zink und zur Bestimmung der Phosphohexose-Isomerase-Aktivität wiedergegeben. Dabei wird besonderer Wert auf eine detaillierte Wiedergabe der Methodik gelegt, um ein Nacharbeiten zu erleichtern. Die Untersuchungen wurden an 334 Patienten für Zink und an 464 Patienten für die Phosphohexose-Isomerase-Aktivität durchgeführt und sind damit auf eine breite Basis gestellt. 1. Es kann festgestellt werden, daß Zink in einer Größenordnung von 40–1300 γ/ml im menschlichen Sperma vorhanden ist. Diese Befunde decken sich mit den Literaturangaben anderer Autoren. Irgendwelche Zusammenhänge mit der morphologischen Qualität des Spermas ließen sich nicht herstellen. 2. Die Phosphohexose-Isomerase-Aktivität steht nach den vorgelegten Befunden eindeutig im Zusammenhang mit der Spermatozoenzahl des Ejaculates und ist von dieser abhängig. Eine Abhängigkeit vom Initialfructosewert war dagegen nicht nachzuweisen. Die Phosphohexose-Isomerase-Aktivitätswerte lagen im Bereich von 10,1–2650 μMol F-6-p/ml/Std. Die Phosphohexose-Isomerase-Aktivität wurde auch bei 58 hormonbehandelten Patienten in vergleichenden Untersuchungen geprüft. Dabei ergab sich bei Testosteron eine deutliche Zunahme der Fermentaktivität. Unter Serum- und Choriongonadotropin war dieser Effekt nicht auszulösen.
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2019-07-16
    Description: Petroleum systems located at passive continental margins received increasing attention in the last decade mainly because of deep- and ultra‐deep-water hydrocarbon exploration and production. The high risks associated with these settings originate mainly from the poor understanding of inherent geodynamic processes. The new priority program SAMPLE (South Atlantic Margin Processes and Links with onshore Evolution), established by the German Science Foundation in 2009 for a total duration of 6 years, addresses a number of open questions related to continental breakup and post‐breakup evolution of passive continental margins. 27 sub‐projects take advantage of the exceptional conditions of the South Atlantic as a prime “Geo‐archive.” The regional focus is set on the conjugate margins located east of Brazil and Argentina on one side and west of Angola, Namibia and South Africa on the other (Figure 1) as well as on the Walvis Ridge and the present‐day hotspot of Tristan da Cunha. The economic relevance of the program is demonstrated by support from several petroleum companies, but the main goal is research on fundamental processes behind the evolution of passive continental margins.
    Repository Name: EPIC Alfred Wegener Institut
    Type: Book , peerRev
    Format: application/pdf
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  • 5
    Publication Date: 2012-08-30
    Description: SUMMARY Elastic Full Waveform Tomography (FWT) aims to reduce the misfit between recorded and modelled data, to deduce a very detailed model of elastic material parameters in the underground. The choice of the elastic model parameters to be inverted affects the convergence and quality of the reconstructed subsurface model. Using the Cross-Triangle-Squares (CTS) model three elastic parametrizations, Lamé parameters m1 = [λ, μ, ρ], seismic velocities m2 = [ V p ,  V s , ρ] and seismic impedances m3 = [ I p ,  I s , ρ] for far-offset reflection seismic acquisition geometries with explosive point sources and free-surface condition are studied. In each CTS model the three elastic parameters are assigned to three different geometrical objects that are spatially separated. The results of the CTS model study reveal a strong requirement of a sequential frequency inversion from low to high frequencies to reconstruct the density model. Using only high-frequency data, cross-talk artefacts have an influence on the quantitative reconstruction of the material parameters, while for a sequential frequency inversion only structural artefacts, representing the boundaries of different model parameters, are present. During the inversion, the Lamé parameters, seismic velocities and impedances could be reconstructed well. However, using the Lamé parametrization -artefacts are present in the λ model, while similar artefacts are suppressed when using seismic velocities or impedances. The density inversion shows the largest ambiguity for all parametrizations. However, the artefacts are again more dominant, when using the Lamé parameters and suppressed for seismic velocity and impedance parametrization. The afore mentioned results are confirmed for a geologically more realistic modified Marmousi-II model. Using a conventional streamer acquisition geometry the P -velocity, S -velocity and density models of the subsurface were reconstructed successfully and are compared with the results of the Lamé parameter inversion.
    Print ISSN: 0956-540X
    Electronic ISSN: 1365-246X
    Topics: Geosciences
    Published by Oxford University Press on behalf of The Deutsche Geophysikalische Gesellschaft (DGG) and the Royal Astronomical Society (RAS).
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  • 6
    Publication Date: 2017-06-15
    Description: ABSTRACT We develop a 2D full waveform inversion approach for the simultaneous determination of S-wave velocity and density models from SH- and Love wave data. We illustrate the advantages of the SH/Love full waveform inversion with a simple synthetic example and demonstrate the method's applicability to a near-surface data set, recorded in the village Cˇ achtice in Northwestern Slovakia. Goal of the survey was to map remains of historical building foundations in a highly heterogeneous subsurface. The seismic survey comprises two parallel SH-profiles with maximum offsets of 24 m and covers a frequency range from 5 Hz to 80 Hz with high signalto-noise ratio well suited for full waveform inversion. Using the Wiechert-Herglotz method we determined a 1D gradient velocity model as a starting model for FWI. The 2D waveform inversion approach uses the global correlation norm as objective function in combination with a sequential inversion of low-pass filtered field data. This mitigates the non-linearity of the multi-parameter inverse problem. Test computations show that the influence of visco-elastic effects on the waveform inversion result is rather small. Further tests using a mono-parameter shear modulus inversion reveal that the inversion of the density model has no significant impact on the final data fit. The final full waveform inversion S-wave velocity and density models show a prominent low-velocity weathering layer. Below this layer the subsurface is highly heterogeneous. Minimum anomaly sizes correspond to approximately half of the dominant Love-wavelength. The results demonstrate the ability of 2D SH waveform inversion to image shallow small scale soil structure. However, they do not show any evidence of foundation walls. This article is protected by copyright. All rights reserved
    Print ISSN: 0016-8025
    Electronic ISSN: 1365-2478
    Topics: Geosciences , Physics
    Published by Wiley-Blackwell
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  • 7
    Publication Date: 2020-02-12
    Keywords: 550 - Earth sciences
    Type: info:eu-repo/semantics/other
    Format: application/pdf
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  • 8
    Publication Date: 2020-02-12
    Description: The Rwenzori Mountains are located within the Albertine Rift Valley in western Uganda. To monitor the microseismic activity in the area we have deployed a seismic network of up to 35 stations for a period of about 20 months. The analysis of the recordings revealed several earthquake clusters within a restricted area NE of the mountain block. The clusters form elongated pipes with 1–2 km diameter and vertical extensions of 3–5 km. Most of them are located in 5–16 km depths; however one cluster reaches down to 22 km. Each cluster is composed of a series of single earthquake swarms with durations between a few days and more than a week, interrupted by intervals of inactivity of up to several months. Some of the swarm events exhibit vertical migration tendencies with estimated velocities between 0.3 and 1 km/day. Local magnitudes range from ML = 0.5 to ML = 4.0 with b-values between 0.96 and 1.2. The source mechanisms of the swarm earthquakes are dominated by normal faulting with tension-axes orientations perpendicular to the rift axis. There are only few strike-slip events and no reverse mechanisms. From petrological considerations we presume that the earthquake swarms are triggered by fluids and gases which originate from a magmatic source below the crust. Melt and/or CO2 are guided along the intersection lines of two steep fault sets that were identified by shear-wave splitting analysis and fault mapping in the Rwenzori area. The existence of a magmatic source within the lithosphere is supported by the detection of a shear-wave velocity reduction in 55–80 km depth from receiver-function analysis and the location of mantle earthquakes at about 60 km. We interpret these observations as indication for an initial rifting process that may eventually lead to the complete detachment of the Rwenzori block from the surrounding rift flanks.
    Language: English
    Type: info:eu-repo/semantics/article
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  • 9
    Publication Date: 2020-12-14
    Description: Mediterranean tectonics since the Lower Cretaceous has been characterized by a multiphase subduction and collision history with temporally and spatially variable, small‐scale plate configurations. A new shear wave velocity model of the Mediterranean upper mantle (MeRE2020), constrained by a very large set of over 200,000 broadband (8–350 s), interstation, Rayleigh wave, phase velocity curves, illuminates the complex structure and fragmentation of the subducting slabs. Phase velocity maps computed using these measurements were inverted for depth‐dependent, shear wave velocities using a stochastic particle‐swarm‐optimization (PSO) algorithm. The resulting three‐dimensional (3‐D) model makes possible an inventory of slab segments across the Mediterranean. Fourteen slab segments of 200–800 km length along‐strike are identified. We distinguish three categories of subducted slabs: attached slabs reaching down to the bottom of the model; shallow slabs of shorter length in downdip direction, terminating shallower than 300 km depth; and detached slab segments. The location of slab segments are consistent with and validated by the intermediate‐depth seismicity, where it is present. The new high‐resolution tomography demonstrates the intricate relationships between slab fragmentation and the evolution of the relatively small and highly curved subduction zones and collisional orogens characteristic of the Mediterranean realm.
    Language: English
    Type: info:eu-repo/semantics/article
    Format: application/pdf
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