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  • 1
    Monograph available for loan
    Monograph available for loan
    Lisse [u.a.] : Balkema
    Call number: 5/M 03.0164
    Type of Medium: Monograph available for loan
    Pages: xiii, 221 S.
    ISBN: 9058092208
    Uniform Title: Géodynamique
    Classification:
    Geophysics
    Language: English
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Keywords: Becken (Geologie) ; Cergy (1996) ; Geologie ; Mittelmeer ; Pannonisches Becken ; Basins (Geology) ; Mediterranean region ; Orogeny ; Alpine region ; Geology, Stratigraphic ; Geology, Cenozoic
    Description / Table of Contents: B. Durand and L. Jolivet: Foreword / Geological Society, London, Special Publications, 156:vii-ix, doi:10.1144/GSL.SP.1999.156.01.01 --- L. Jolivet, D. Frizon de Lamotte, A. Mascle, and M. Séranne: The Mediterranean Basins: Tertiary Extension within the Alpine Orogen — an introduction / Geological Society, London, Special Publications, 156:1-14, doi:10.1144/GSL.SP.1999.156.01.02 --- Western Mediterranean --- Michel Séranne: The Gulf of Lion continental margin (NW Mediterranean) revisited by IBS: an overview / Geological Society, London, Special Publications, 156:15-36, doi:10.1144/GSL.SP.1999.156.01.03 --- N. Chamot-Rooke, J.-M. Gaulier, and F. Jestin: Constraints on Moho depth and crustal thickness in the Liguro-Provençal basin from a 3D gravity inversion: geodynamic implications / Geological Society, London, Special Publications, 156:37-61, doi:10.1144/GSL.SP.1999.156.01.04 --- J. Vergés and F. Sàbat: Constraints on the Neogene Mediterranean kinematic evolution along a 1000 km transect from Iberia to Africa / Geological Society, London, Special Publications, 156:63-80, doi:10.1144/GSL.SP.1999.156.01.05 --- A. Benedicto, M. Séguret, and P. Labaume: Interaction between faulting, drainage and sedimentation in extensional hanging-wall syncline basins: example of the Oligocene Matelles basin (Gulf of Lion rifted margin, SE France) / Geological Society, London, Special Publications, 156:81-108, doi:10.1144/GSL.SP.1999.156.01.06 --- H. P. Zeck: Alpine plate kinematics in the western Mediterranean: a westward-directed subduction regime followed by slab roll-back and slab detachment / Geological Society, London, Special Publications, 156:109-120, doi:10.1144/GSL.SP.1999.156.01.07 --- Alain Mascle and Roland Vially: The petroleum systems of the Southeast Basin and Gulf of Lion (France) / Geological Society, London, Special Publications, 156:121-140, doi:10.1144/GSL.SP.1999.156.01.08 --- Marjorie Wilson and Gianluca Bianchini: Tertiary-Quaternary magmatism within the Mediterranean and surrounding regions / Geological Society, London, Special Publications, 156:141-168, doi:10.1144/GSL.SP.1999.156.01.09 --- A. Mauffret and I. Contrucci: Crustal structure of the North Tyrrhenian Sea: first result of the multichannel seismic LISA cruise / Geological Society, London, Special Publications, 156:169-193, doi:10.1144/GSL.SP.1999.156.01.10 --- Pannonian Basin --- Frank Horváth and Gábor Tari: IBS Pannonian Basin project: a review of the main results and their bearings on hydrocarbon exploration / Geological Society, London, Special Publications, 156:195-213, doi:10.1144/GSL.SP.1999.156.01.11 --- Gábor Tari, Péter Dövényi, István Dunkl, Frank Horváth, László Lenkey, Mihai Stefanescu, Péter Szafián, and Tamás Tóth: Lithospheric structure of the Pannonian basin derived from seismic, gravity and geothermal data / Geological Society, London, Special Publications, 156:215-250, doi:10.1144/GSL.SP.1999.156.01.12 --- István Györfi, László Csontos, and András Nagymarosy: Early Tertiary structural evolution of the border zone between the Pannonian and Transylvanian Basins / Geological Society, London, Special Publications, 156:251-267, doi:10.1144/GSL.SP.1999.156.01.13 --- P. Gerner, G. Bada, P. Dövényi, B. Müller, M. C. Oncescu, S. Cloetingh, and F. Horváth: Recent tectonic stress and crustal deformation in and around the Pannonian Basin: data and models / Geological Society, London, Special Publications, 156:269-294, doi:10.1144/GSL.SP.1999.156.01.14 --- László Fodor, László Csontos, Gábor Bada, István Györfi, and László Benkovics: Tertiary tectonic evolution of the Pannonian Basin system and neighbouring orogens: a new synthesis of palaeostress data / Geological Society, London, Special Publications, 156:295-334, doi:10.1144/GSL.SP.1999.156.01.15 --- E. Juhász, L. Phillips, P. Müller, B. Ricketts, Á. Tóth-Makk, M. Lantos, and L. Ó. Kovács: Late Neogene sedimentary facies and sequences in the Pannonian Basin, Hungary / Geological Society, London, Special Publications, 156:335-356, doi:10.1144/GSL.SP.1999.156.01.16 --- Marco Sacchi, Frank Horváth, and Orsolya Magyari: Role of unconformity-bounded units in the stratigraphy of the continental record: a case study from the Late Miocene of the western Pannonian Basin, Hungary / Geological Society, London, Special Publications, 156:357-390, doi:10.1144/GSL.SP.1999.156.01.17 --- R. T. Van Balen, L. Lenkey, F. Horváth, and S. A. P. L. Cloetingh: Two-dimensional modelling of stratigraphy and compaction-driven fluid flow in the Pannonian Basin / Geological Society, London, Special Publications, 156:391-414, doi:10.1144/GSL.SP.1999.156.01.18 --- Eastern Mediterranean --- Denis Hatzfeld: The present-day tectonics of the Aegean as deduced from seismicity / Geological Society, London, Special Publications, 156:415-426, doi:10.1144/GSL.SP.1999.156.01.19 --- L. Jolivet and M. Patriat: Ductile extension and the formation of the Aegean Sea / Geological Society, London, Special Publications, 156:427-456, doi:10.1144/GSL.SP.1999.156.01.20 --- A. L. W. Lips, J. R. Wijbrans, and S. H. White: New insights from 40Ar/39Ar laserprobe dating of white mica fabrics from the Pelion Massif, Pelagonian Zone, Internal Hellenides, Greece: implications for the timing of metamorphic episodes and tectonic events in the Aegean region / Geological Society, London, Special Publications, 156:457-474, doi:10.1144/GSL.SP.1999.156.01.21 --- Aral I. Okay and Okan Tüysüz: Tethyan sutures of northern Turkey / Geological Society, London, Special Publications, 156:475-515, doi:10.1144/GSL.SP.1999.156.01.22 --- General --- P. A. Ziegler and F. Roure: Petroleum systems of Alpine-Mediterranean foldbelts and basins / Geological Society, London, Special Publications, 156:517-540, doi:10.1144/GSL.SP.1999.156.01.23 --- C. Doglioni, E. Gueguen, P. Harabaglia, and F. Mongelli: On the origin of west-directed subduction zones and applications to the western Mediterranean / Geological Society, London, Special Publications, 156:541-561, doi:10.1144/GSL.SP.1999.156.01.24
    Pages: Online-Ressource (IX, 569 Seiten) , Illustrationen, Diagramme, Karten
    ISBN: 1862390339
    Language: English
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  • 3
    Electronic Resource
    Electronic Resource
    Oxford, UK : Blackwell Science Ltd
    Terra nova 9 (1997), S. 0 
    ISSN: 1365-3121
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: In the Central Mediterranean two back-arc basins, the Liguro-Provençal (LPb) and the Tyrrhenian basin (Tb), opened progressively and consecutively from the late Eocene–Oligocene to the present. Evolution in space and time of rifting and drifting processes, along three different transects across these basins, shows differences in the style of extension: LPb opened with the formation of a narrow, single rift, while in the Tb deformation and magmatism is spread over a wide area. Moreover at the Northern end of the Tb the locus of extension progressively migrated towards the east whereas in the Southern Tb the locus of extension and magmatism migrated inside the basin, inducing continental break-up and drifting of the previously formed older conjugate basins. We propose that these different styles of back-arc extension depend upon internal conditions, such as prerift rheology linked with its geological heritage, and external conditions, e.g. the style of subduction.
    Type of Medium: Electronic Resource
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  • 4
    Publication Date: 2007-10-08
    Description: The northwestern part of Holsnoy island, in the Bergen Arcs, Norway, consists of a granulite-facies protolith partially transformed at depth in eclogite (700 {degrees}C, > 19 kbars) and amphibolite (650 {degrees}C, 8-10 kbars) facies during the Caledonian orogenesis. Eclogitized zones are mainly planar objects (fractures with parallel reaction bands and cm-to-100 m-scale shear zones). Eclogitic zones are distributed in two sets of orientations and the associated deformation can be described as bookshelf tectonics'. The major shear zones strike around N120 and dip to the North, and show consistent top-to-the-NE shear sense throughout the area. In the large-scale kinematic frame of Caledonian NW-dipping slab, eclogitic shear zones are interpreted as the way to detach crustal units from the subducting slab and to prevent their further sinking. As the retrograde amphibolitic deformation pattern is similar to the eclogitic one, the detached crustal units started their way up along these eclogitic shear zones. Radiometric ages of eclogitic and amphibolitic metamorphism and their comparison with the chronology of Caledonian orogenesis show that the deformation recorded on Holsnoy occurred in a convergent context. The mechanism we propose can thus account for the first steps of exhumation during collision.
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  • 5
    Publication Date: 2007-10-08
    Description: In SW Turkey, Fe-Mg-carpholite has recently been recognized in the basal metasediments of the Lycian Nappes, which overthrust the Menderes Massif on its southern flank. This high-pressure-low-temperature (HP-LT) metamorphic index mineral was widely found in the Bodrum peninsula region. Our new metamorphic and structural data on similar carpholite-bearing rocks found farther north in several klippen of the Lycian Nappes located on top of the Menderes Massif show that HP-LT rocks in SW Turkey occur over a distance of 〉200 km in both north-south and east-west directions, thus indicating a wide HP-LT metamorphic belt. The deformation pattern from the Bodrum peninsula to Civril, all along the contact between the Lycian Nappes and the Menderes Massif, reveals the role played by major top-to-the-NE shear zones contemporaneous with exhumation of the Lycian HP-LT rocks. This deformation shows an oblique direction of opposite shear sense relative to the earlier southward translation of the Lycian Nappes over the Menderes Massif, for which top-to-the-south displacements are preserved in the upper units of the Lycian Nappes on the Bodrum peninsula, as well as at the base of the Lycian nappe klippen located farther north. The widespread distribution of well-preserved Fe-Mg-carpholite-bearing rocks in the Lycian Nappes has implications for the geometry of the accretionary wedge responsible for HP-LT metamorphism in SW Turkey.
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  • 6
    Publication Date: 2009-04-30
    Description: The Apennine belt represents a typical orogenic segment of the western Mediterranean, characterized by the tectonic convergence between European and Africa plates after oceanic subduction. Both oceanic- and continent-derived metamorphic complexes, considered as the remnants of the subduction-exhumation cycle, crop out in the inner sectors of the Apennine belt, where extensional deformation has dominated since the Early Oligocene. We review the available structural, metamorphic and geochronological data coming from these metamorphic complexes in order to provide a kinematics reconstruction accounting for the tectono-metamorphic evolution of the Apennines, from oceanic subduction to final extensional reworking. During the Eocene, oceanic rocks were progressively subducted down to eclogite-facies conditions following a subduction-type metamorphic gradient. The transition from oceanic- to continental-subduction was coeval with a transition from subduction-type to Barrovian-type metamorphic gradient. Continental collision, at the Eocene-Oligocene boundary, post-dated the syn-orogenic exhumation of HP-rocks and was synchronous with the onset of post-orogenic extension in the hinterland domains. Extensional deformation migrated to the east, following the forelandward migration of the thrust system at the trench. The concomitance of extension and compression is here related to fast rollback of the subducting plate and delamination of the lithospheric mantle below the subducted continental crust. Implications on how the subduction tectonics, syn-orogenic exhumation and post-orogenic extension could have controlled the circulation of HP-rocks in the developing Apennines are also discussed.
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  • 7
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  • 9
    Publication Date: 2018-02-09
    Electronic ISSN: 1553-040X
    Topics: Geosciences
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  • 10
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