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  • 2005-2009  (5)
  • 2000-2004  (11)
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  • 1
    Call number: 9/M 07.0372
    In: Geological Society special publication
    Description / Table of Contents: Imaging, mapping and modelling continental lithosphere extension and breakup: an introduction, G D Karner, G Manatschal and L M Pinheiro. - Break-up of the Newfoundland-Iberia rift, B E Tucholke, D S Sawyer and J-C Sibuet. - Structure of the Flemish Cap margin, Newfoundland: insights into mantle and crustal processes during continental breakup, J R Hopper, T Funck and B E Tucholke. - Early Cretaceous motion of Flemish Cap with respect to North America: implications on the formation of Orphan Basin and SE Flemish Cap-Galicia Bank conjugate margins, J-C Sibuet, S P Srivastava, M Enachescu and G D Karner. - The formation of non-volcanic rifted margins by the progressive extension of the lithosphere: the example of the West Iberian margin, T J Reston. - Roles of lithospheric strain softening and heterogeneity in determining the geometry of rifts and continental margins, R S Huismans and C Beaumont. - The role of gravitational instabilities, density structure, and extension rate in the evolution of continental margins, E Burov. - A dynamic model of rifting between Galicia Bank and Flemish Cap during opening of the North Atlantic Ocean, D L Harry and S Grandell. - A kinematic modelling approach to lithosphere deformation and basin formation: application to the Black Sea, S S Egan and D J Meredith. - Early kinematic history of the Goban Spur rifted margin derived from a new model of continental breakup and sea-floor spreading initiation, D Healy and N J Kusznir. - The boundary between continental rifting and seafloor spreading in the Woodlark Basin, Papua New Guinea, A M Goodliffe and B Taylor. - Nature of the continent-ocean transition zone along the southern Australian continental margin: a comparison of the Naturaliste Plateau, SW Australia, and the central Great Australian Bight sectors, N G Direen, I Borissova, H M J Stagg, J B Colwell and P A Symonds. - Constraints on the deformation and rupturing of continental lithosphere of the Red Sea: the transition from rifting to drifting, J R Cochran and G D Karner. - Observations from the Alpine Tethys and Iberia Newfoundland margins pertinent to the interpretation of continental breakup, G Manatschal, O Muntener, L L Lavier, T A Minshull and G Peron-Pinvidic. - Overview of tectonic settings related to the rifting and opening of Mesozoic ocean basins in the Eastern Tethys: Oman, Himalayas and Eastern Mediterranean regions, A H F Robertson. - Continental lithospheric thinning and breakup in response to upwelling divergent mantle flow: application to the Woodlark, Newfoundland, and Iberia margins, N J Kusznir G D Karner. - Observations from the Basin and Range Province (western United States) pertinent to the interpretation of regional detachment faults, N Christie-Blick, M H Anders, S Wills, C D Walker and B Renik. - Effects of initial weakness on rift architecture, S Dyksterhuis, P Rey, R D Müller and L Moresi. - Incompressible viscous formulations for deformation and yielding of the lithosphere, L Moresi, H-B Muhlhaus, V Lemiale and D May.
    Type of Medium: Monograph available for loan
    Pages: vi, 482 S.
    ISBN: 1862392285
    Series Statement: Geological Society special publication 282
    Classification:
    Lithosphere
    Location: Reading room
    Branch Library: GFZ Library
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  • 2
    Call number: M 04.0414 ; M 04.0514
    Description / Table of Contents: Traditionally, investigations of the rheology and deformation of the lithosphere (the rigid or mechanically strong outer layer of the Earth, which contains the crust and the uppermost part of the mantle) have taken place at one scale in the laboratory and at an entirely different scale in the field. Laboratory experiments are generally restricted to centimeter-sized samples and day- or year-length times, while geological processes occur over tens to hundreds of kilometers and millions of years. The application of laboratory results to geological systems necessitates extensive extrapolation in both temporal and spatial scales, as well as a detailed understanding of the dominant physical mechanisms. The development of an understanding of large-scale processes requires an integrated approach.
    Type of Medium: Monograph available for loan
    Pages: xii, 352 S. , 26 cm
    ISBN: 0231127391
    Series Statement: MARGINS theoretical and experimental earth science series
    Classification:
    Petrophysics
    Location: Upper compact magazine
    Location: Upper compact magazine
    Branch Library: GFZ Library
    Branch Library: GFZ Library
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  • 3
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    PANGAEA
    In:  Supplement to: Goodliffe, Andrew M; Taylor, Brian; Karner, Garry D (2001): Correlations between seismic, logging, and core data from ODP Leg 180 sites in the western Woodlark Basin. In: Huchon, P; Taylor, B; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 180, 1-25, https://doi.org/10.2973/odp.proc.sr.180.167.2001
    Publication Date: 2024-01-09
    Description: Synthetic seismograms are constructed from check shot-corrected velocity and density measurements collected during Ocean Drilling Program (ODP) Leg 180 at Sites 1109, 1115, and 1118. The synthetic seismograms facilitate direct correlation of a coincident multichannel seismic (MCS) profile with borehole data collected at the three sites. The MCS data and the synthetic seismograms correlate very well, with most major reflectors successfully reproduced in the synthetics. Our results enable a direct calibration of the MCS data in terms of age, paleoenvironment, and subsidence history. Seismic reflectors are time correlative within stratigraphic resolution but are often observed to result from different lithologies across strike. Our results facilitate the extrapolation of the sedimentation history into an unsampled section of Site 1118 and enable a full correlation between the three sites using all the data collected during ODP Leg 180. This study forms the foundation for regionalizing the site data to the northern margin of the Woodlark Basin, where the transition from continental rifting to seafloor spreading is taking place.
    Keywords: Ocean Drilling Program; ODP
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 4
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    Unknown
    PANGAEA
    In:  Supplement to: Cook, Alan C; Karner, Garry D (2002): Data report: Organic petrology of Leg 180 samples, western Woodlark Basin, Papua New Guinea. In: Huchon, P; Taylor, B; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 180, 1-35, https://doi.org/10.2973/odp.proc.sr.180.157.2002
    Publication Date: 2024-01-09
    Description: Seventy-one samples from Ocean Drilling Program Leg 180 sites were analyzed for vitrinite reflectance and organic type. The objective was to define maximum paleotemperatures across the western Woodlark Basin as a function of depth. The organic matter is of early Pliocene to Holocene age and was recovered from drilled depths of 4.5 to 851.3 meters below seafloor. Organic matter is generally restricted to woody fragments within the sediment, although in a number of fine-grained samples, organic matter is dispersed throughout the sample. Virtually all samples contain vitrinite, part of which may be derived from drifted logs. One sample was found to be barren of organic matter, and two contain only fusinite and semifusinite. Variation of vitrinite reflectance is not systematic with either depth or location, and it appears that formation temperatures have been insufficient to cause an increase in vitrinite reflectance levels. Textural variations within the vitrinite show better correlation with depth. Samples of hypautochthonous peats represent either a terrestrial phase of sedimentation or large peat intraclasts within the section, possibly produced by forest fires in the source areas of the organic matter. The vitrinite and peat-derived samples appear to come from eucalyptus forest settings away from the coastline. Liptinite is not abundant in most of the samples (excluding suberinite associated with woody tissues). Marine liptinite is rare to absent, although many of the samples contain abundant foraminiferal tests. Pyrite is abundant in many of the wood fragments, and some pyritization of woody tissues has taken place.
    Keywords: 180-1108B; 180-1109C; 180-1109D; 180-1114A; 180-1115A; 180-1115B; 180-1115C; 180-1116A; 180-1118A; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Elevation of event; Event label; Joides Resolution; Latitude of event; Leg180; Longitude of event; Microphotometer LEITZ MPV 1.1; Ocean Drilling Program; ODP; Sample amount; Sample comment; Sample ID; Solomon Sea; Vitrinite reflection
    Type: Dataset
    Format: text/tab-separated-values, 388 data points
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  • 5
    Publication Date: 2024-01-09
    Keywords: 180-1118; Age, dated; Age, dated standard deviation; Ageprofile Datum Description; COMPCORE; Composite Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Joides Resolution; Leg180; Ocean Drilling Program; ODP; Solomon Sea; Two-way traveltime
    Type: Dataset
    Format: text/tab-separated-values, 116 data points
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  • 6
    Publication Date: 2024-01-09
    Keywords: 180-1109; Age, dated; Age, dated standard deviation; Ageprofile Datum Description; COMPCORE; Composite Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Joides Resolution; Leg180; Ocean Drilling Program; ODP; Solomon Sea; Two-way traveltime
    Type: Dataset
    Format: text/tab-separated-values, 215 data points
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  • 7
    Publication Date: 2024-01-09
    Keywords: 180-1115; Age, dated; Age, dated standard deviation; Ageprofile Datum Description; COMPCORE; Composite Core; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; Joides Resolution; Leg180; Ocean Drilling Program; ODP; Solomon Sea; Two-way traveltime
    Type: Dataset
    Format: text/tab-separated-values, 245 data points
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  • 8
    Publication Date: 2003-12-01
    Print ISSN: 0012-821X
    Electronic ISSN: 1385-013X
    Topics: Geosciences , Physics
    Published by Elsevier
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  • 9
    Publication Date: 2004-04-01
    Print ISSN: 0012-821X
    Electronic ISSN: 1385-013X
    Topics: Geosciences , Physics
    Published by Elsevier
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  • 10
    Publication Date: 2006-05-01
    Print ISSN: 0264-8172
    Electronic ISSN: 1873-4073
    Topics: Geosciences
    Published by Elsevier
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