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  • 1
    Call number: AR 99.0297
    Type of Medium: GFZ publications
    Pages: 172 S.
    Classification:
    Petrophysics
    Branch Library: GFZ Library
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  • 2
    Call number: G 8815
    Type of Medium: Monograph available for loan
    Pages: XV, 327 S. : graph. Darst.
    Note: Basel, Univ., Diss., 1986
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Monograph available for loan
    Monograph available for loan
    Cambridge [u.a.] : MIT Press
    Call number: PIK N 411-07-0195 ; M 07.0288 ; 9/M 07.0289
    Description / Table of Contents: Contents: Tectonic Faults: Agents of Change on a Dynamic Earth. - Fault Zones from Top to Bottom . - Nucleation and Growth of Fault Systems. - Seismic Fault Rheology and Earthquake Dynamics. - Continental Fault Structure and Rheology from the Frictional-to-Viscous Transition Downwards. - Group Report: Rheology of Fault Rocks and Their Surroundings. - Topography, Denudation, and Deformation: The Role of Surface Processes on Fault Evolution. - Constraining the Denudational Response to Faulting. - Surface Environmental Effects on and of Faulting. - Fluid Processes in Deep Crustal Fault Zones. - Deformation in the Presence of Fluids and Mineral Reactions: Effect of Fracturing and Fluid Rock Interaction on Seismic Cycles. - On the Effects of Melting on Faulting and Continental Deformation. - Fluids, Geochemical Cycles, and Mass Transport in Fault Zones.
    Type of Medium: Monograph available for loan
    Pages: xiii, 446 S.
    ISBN: 9780262083621
    Series Statement: Dahlem workshop report 95
    Classification:
    Tectonics
    Location: A 18 - must be ordered
    Location: Upper compact magazine
    Location: Reading room
    Branch Library: PIK Library
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 4
    Publication Date: 2019-12-05
    Description: The AlpArray programme is a multinational, European consortium to advance our understanding of orogenesis and its relationship to mantle dynamics, plate reorganizations, surface processes and seismic hazard in the Alps–Apennines–Carpathians–Dinarides orogenic system. The AlpArray Seismic Network has been deployed with contributions from 36 institutions from 11 countries to map physical properties of the lithosphere and asthenosphere in 3D and thus to obtain new, high-resolution geophysical images of structures from the surface down to the base of the mantle transition zone. With over 600 broadband stations operated for 2 years, this seismic experiment is one of the largest simultaneously operated seismological networks in the academic domain, employing hexagonal coverage with station spacing at less than 52 km. This dense and regularly spaced experiment is made possible by the coordinated coeval deployment of temporary stations from numerous national pools, including ocean-bottom seismometers, which were funded by different national agencies. They combine with permanent networks, which also required the cooperation of many different operators. Together these stations ultimately fill coverage gaps. Following a short overview of previous large-scale seismological experiments in the Alpine region, we here present the goals, construction, deployment, characteristics and data management of the AlpArray Seismic Network, which will provide data that is expected to be unprecedented in quality to image the complex Alpine mountains at depth.
    Description: Published
    Description: 1009–1033
    Description: 1T. Struttura della Terra
    Description: JCR Journal
    Keywords: Seismology ; Alps ; Seismic network ; Geodynamics ; Seismic imaging ; Mountain building
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 5
    Publication Date: 2021-07-05
    Description: We investigate the evolution of the three‐dimensional thermal structure of a palaeo‐subduction channel exposed in the Penninic units of the central Tauern Window (Eastern Alps). Structural and petrological observations reveal a sheath fold with an amplitude of some 20 km that formed under high‐P conditions (~2 GPa). The fold is a composite structure that isoclinally folded the thrust of an ophiolitic nappe derived from Alpine Tethys Ocean onto a unit of the distal European continental margin, also affected by the high‐P conditions. This structural assemblage is preserved between two younger domes at either end of the Tauern Window. The domes deform isograds of the T‐dominated Barrovian metamorphism that itself overprints the high‐P metamorphism partly preserved in the sheath fold. Using Raman spectroscopy on carbonaceous material (RSCM), we are able to distinguish peak‐temperature domains related to the original subduction metamorphism from domains associated with the later temperature‐dominated (Barrovian) metamorphism. The distribution of RSCM temperatures in the Barrovian domain indicates a lateral and vertical decrease of peak temperature with increasing distance from the centres of the thermal domes. This represents a downward increase of palaeo‐temperature, in line with previous studies. However, we observe the opposite palaeo‐temperature trend in the lower limb of the sheath fold, namely an upward increase. We interpret this inverted palaeo‐temperature domain as the relic of a subduction‐related temperature field. Towards the central part of the sheath fold's upper limb, RSCM temperatures increase to a maximum of ~520°C. Further upsection in the hangingwall of the sheath fold, palaeo‐peak temperatures decrease to where they are indistinguishable from the peak temperatures of the overprinting Barrovian metamorphism. Peak‐temperature contours of the subduction‐related metamorphism are oriented roughly parallel to the folded nappe contacts and lithological layering. The contours close towards the northern, western and eastern parts of the fold, resulting in an eye‐shaped, concentric pattern in cross‐section. The temperature contour geometry therefore mimics the fold geometry itself, indicating that these contours were also folded in a sheath‐like manner. We propose that this sheath‐like pattern is the result of a two‐stage process that reflects a change of the mode of nappe formation in the subduction zone from thrusting to fold nappe formation. First, thrusting of a hot oceanic nappe onto a colder continental nappe created an inverted peak‐thermal gradient. Second, sheath folding of this composite nappe structure together with the previously established peak‐temperature pattern during exhumation. This pattern was preserved because temperatures decreased during retrograde exhumation metamorphism and remained less than the subduction‐related peak temperatures during the later Barrovian overprint. The fold ascended with diapir‐like kinematics in the subduction channel.
    Description: Deutsche Forschungsgemeinschaft http://dx.doi.org/10.13039/501100001659
    Keywords: 552.4 ; RSCM ; sheath fold ; subduction metamorphism ; subduction‐exhumation channel ; temperature field
    Type: article
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  • 6
    Publication Date: 2021-07-04
    Description: We investigate a well‐preserved paleo subduction channel that preserves a coherent part of the European continental margin exposed in the central Tauern Window (Eastern Alps), with the aim of testing models of sheath fold nappe formation and exhumation. The subduction zone was active during Paleogene convergence of the European and Adriatic plates, after closure of the Alpine Tethyan ocean. New cross sections and structural data together with new petrological data document a recumbent, tens of kilometers‐scale sheath fold in the center of the Tauern Window that formed during pervasive top‐foreland shear while subducted at high‐pressure (HP) conditions (~2.0 GPa, 500 °C) close to maximum burial depth. The fold comprises an isoclinally folded thrust that transported relicts of the former Alpine Tethys onto a distal part of the former European continental margin. The passive margin stratigraphy is still well preserved in the fold and highlights the special character of this segment of the European continental margin. We argue that this segment formed a promontory to the margin, which was inherited from Mesozoic rifting. In accordance with classical sheath fold theory, this promontory may have acted as an initial structural perturbation to nucleate a fold that was passively amplified to a sheath fold during top‐foreland shear in the subduction zone. The fold was at least partly exhumed and juxtaposed with the surrounding lower pressure units by opposing top‐hinterland and top‐foreland shear zones above and below, respectively, that is, in the sense of a nappe fold formed during channel‐extrusion exhumation.
    Description: Key Points: The central Tauern Window preserves a crustal‐scale sheath fold that formed in the Alpine subduction zone in top‐foreland shear. The sheath fold was formed by passive amplification of a rift‐inherited heterogeneity of the European margin. Exhumation of sheath fold nappe from HP conditions was achieved at least partly by channel extrusion.
    Description: Deutsche Forschungsgemeinschaft (DFG) http://dx.doi.org/10.13039/501100001659
    Keywords: 551.8 ; sheath fold ; exhumation ; high‐pressure metamorphism ; Alps ; channel extrusion ; orogenic wedge
    Type: article
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  • 7
    Publication Date: 2021-03-29
    Description: Granitic gneisses of the Central Aar Granite host a shear zone network that formed at greenschist facies conditions. The work area is located in the Bächlital (Grimsel area, Central Switzerland) and was chosen for the analysis of shear zones because of the weakly anisotropic fabric of the host gneisses. Contrary to previous publications (e.g. Choukroune & Gapais, 1983), none of these host rocks are undeformed. They contain a penetrative foliation (S1) that strikes consistently ENE-WSW with a steep dip of around 70° to the south. This foliation is overprinted by the aforementioned shear zone network, which was the main focus of this study...
    Description: conference
    Keywords: 551 ; VAE 140 ; VKA 200 ; VKB 291 ; VEB 168 ; VKB 230 ; VKB 270 ; Gesteinsdeformation {Strukturgeologie} ; Gefügekunde der Gesteine ; Metamorphe Komplexe, Alpen {Petrologie} ; Schweizer Alpen {Geologie} ; Metamorphite aus sauren bis intermediären Edukten {Petrologie} ; Produkte mechanischer Deformation {Petrologie} ; Aarmassiv ; Scherzone ; Granitgneis ; Feldspäte ; Deformation 〈Geologie〉
    Language: German
    Type: anthologyArticle , publishedVersion
    Format: application/pdf
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  • 8
    Publication Date: 2023-02-01
    Description: The mountain chains of the Central Mediterranean (the Apennines, the Alps, the Dinarides, the Albanides, and the Hellenides) are shaped by complex tectonics arising from the motion and collision of several microplates. Intense onshore and offshore seismic activity puts the rich cultural heritage characterising the entire region at risk. A better understanding of the lithospheric structures and knowledge of the interaction between different tectonic units is key to unraveling the processes underlying seismic activity in this area. In recent years, top-quality seismological data from several groundbreaking experiments have yielded new insight into the orogenic systems of the region (e.g., IberArray, AlpArray, and its complementary seismic experiments, or the “THALES WAS RIGHT” EU project). Similar projects are planned to cover other parts of this critical region, for example, AdriaArray, which will cover the Adria microplate and the Balkans with a dense seismological array.
    Description: Published
    Description: 1003668
    Description: 5TM. Informazione ed editoria
    Description: JCR Journal
    Repository Name: Istituto Nazionale di Geofisica e Vulcanologia (INGV)
    Type: article
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  • 9
  • 10
    Publication Date: 2020-10-29
    Description: We study the crustal structure under the Eastern and Southern Alps using ambient noise tomography. We use cross-correlations of ambient seismic noise between pairs of 71 permanent stations and 19 stations of the Eastern Alpine Seismic Investigation (EASI) profile to derive new 3D shear velocity models for the crust. Continuous records from 2014 and 2015 are cross-correlated to estimate Green's functions of Rayleigh and Love waves propagating between the station pairs. Group velocities extracted from the cross-correlations are inverted to obtain isotropic 3D Rayleigh- and Love-wave shear-wave velocity models. Our models image several velocity anomalies and contrasts and reveal details of the crustal structure. Velocity variations at short periods correlate very closely with the lithologies of tectonic units at the surface and projected to depth. Low-velocity zones, associated with the Po and Molasse sedimentary basins, are imaged well to the south and north of the Alps, respectively. We find large high-velocity zones associated with the crystalline basement that forms the core of the Tauern Window. Small-scale velocity anomalies are also aligned with geological units of the Austroalpine nappes. Clear velocity contrasts in the Tauern Window along vertical cross sections of the velocity model show the depth extent of the tectonic units and their bounding faults. A mid-crustal velocity contrast is interpreted as a manifestation of intracrustal decoupling in the Eastern Alps that accommodated eastward escape of the Alcapa block.
    Print ISSN: 1869-9510
    Electronic ISSN: 1869-9529
    Topics: Geosciences
    Published by Copernicus on behalf of European Geosciences Union.
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