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  • 2010-2014  (238)
  • 1990-1994  (106)
  • 1985-1989  (118)
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Keywords
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Year
  • 1
    Monograph available for loan
    Monograph available for loan
    Subduction zones; Part I (1988)
    Basel : Birkhäuser
    Associated volumes
    Details Availability
    Call number: G 9097/1
    In: Subduction zones
    Type of Medium: Monograph available for loan
    Pages: Seiten 449 - 800 , Illustrationen, Diagramme
    ISBN: 3-7643-1928-3 , 0-8176-1928-3
    URL: https://link.springer.com/journal/24/128/3
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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    BOOK
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  • 2
    Monograph available for loan
    Monograph available for loan
    Subduction zones; Part II (1989)
    Basel : Birkhäuser
    Associated volumes
    Details Availability
    Call number: G 9097/2
    In: Subduction zones
    Type of Medium: Monograph available for loan
    Pages: 282 Seiten , Illustrationen, Diagramme
    ISBN: 3-7643-2272-1 , 0-8176-2272-1
    URL: https://link.springer.com/journal/24/129/1
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 3
    Unknown
    Subduction Zones, Part II (1989)
    Basel, Boston, Berlin : Birkhäuser
    Details
    Description / Table of Contents: Subduction zones consume oceanic lithosphere and are an indispensible part of plate tectonics. Unlike the oceanic lithosphere production system which can be linked as a nearly continuous, albeit sinuous, strand around the earth, subduction zones are a rather dissociated group and are found in several isolated corners of the world. While plate tectonics can predict that subduction zones are required along certain plate boundaries, it does not stipulate how subduction zones initiate and develop. The preservation of newly created oceanic lithosphere and the propensity for spreading centers to fragment continents leaves a wealth of geological informa­ tion on the initiation and evolution of spreading. On the other hand, the subject of subduction initiation has little observational basis. To find such observations, we need to look at some muddled tectonic regimes. The Macquarie Ridge complex presents a natural laboratory for studies of subduction initiation. 2. Tectonics of the Macquarie Ridge Complex The Macquarie Ridge complex is a complicated physiographic feature that trends approximately north-south between South Island, New Zealand and the Pacific-Antarctica spreading center. This feature consists of a sequence of troughs and ridges, with Macquarie Island as the only exposed expression. The seismically active Macquarie Ridge complex (hereafter: MRC) is crudely continuous with the Tonga-Kermadec-New Zealand seismic activity. The basic physiographic features and seismicity of the MRC are shown in Figure I. The earthquake epicenters generally cluster about the bathymetric expression of the MRC.
    Pages: Online-Ressource (V, 282 Seiten)
    ISBN: 9783034891400
    URL: http://link.springer.com/journal/24/129/1/
    Language: English
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    E-BOOK
  • 4
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    Biogeochemical measurements of cold seep sediments inhabit by vesicomyid clams in the Japan Deep Sea Trench (2014)
    PANGAEA
    In:  Supplement to: Felden, Janine; Ruff, S Emil; Ertefai, Tobias F; Inagaki, Fumio; Hinrichs, Kai-Uwe; Wenzhöfer, Frank (2014): Anaerobic methanotrophic community of a 5346 m-deep vesicomyid clam colony in the Japan Trench. Geobiology, https://doi.org/10.1111/gbi.12078
    Details
    Publication Date: 2023-06-08
    Description: Vesicomyidae clams harbor sulfide-oxidizing endosymbionts and are typical members of cold seep communities associated with tectonic faults where active venting of fluids and gases takes place. We investigated the central biogeochemical processes that supported a vesicomyid clam colony as part of a locally restricted seep community in the Japan Trench at 5346 m water depth, one of the deepest seep settings studied to date. An integrated approach of biogeochemical and molecular ecological techniques was used combining in situ and ex situ measurements. During the cruise YK06-05 in 2006 with the RV Yokosuka to the Japan Trench, we investigated a clam colony inhabited by Abyssogena phaseoliformis (former known as Calyptogena phaseoliformis) and Isorropodon fossajaponicum (former known as Calyptogena fossajaponica). The targeted sampling and precise positioning of the in situ instruments were achieved with the manned research submersible Shinkai 6500 (JAMSTEC, Nankoku, Kochi, Japan). Sampling was first performed close to the rim of the JTC colony and then at the center. Immediately after sample recovery onboard, the sediment core was sub-sampled for ex situ rate measurements or preserved for later analyses. In sediment of the clam colony, low sulfate reduction (SR) rates (max. 128 nmol ml**-1 d**-1) were coupled to the anaerobic oxidation of methane (AOM). They were observed over a depth range of 15 cm, caused by active transport of sulfate due to bioturbation of the vesicomyid clams. A distinct separation between the seep and the surrounding seafloor was shown by steep horizontal geochemical gradients and pronounced microbial community shifts. The sediment below the clam colony was dominated by anaerobic methanotrophic archaea (ANME-2c) and sulfate-reducing Desulfobulbaceae (SEEP-SRB-3, SEEP-SRB-4). Aerobic methanotrophic bacteria were not detected in the sediment and the oxidation of sulfide seemed to be carried out chemolithoautotrophically by Sulfurovum species. Thus, major redox processes were mediated by distinct subgroups of seep-related microorganisms that might have been selected by this specific abyssal seep environment. Fluid flow and microbial activity was low but sufficient to support the clam community over decades and to build up high biomasses. Hence, the clams and their microbial communities adapted successfully to a low-energy regime and may represent widespread chemosynthetic communities in the Japan Trench.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 9 datasets
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    DATA PANGAEA
  • 5
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    Archaeal and bacterial diversity at different sites as determined by 16S rRNA gene analysis (2013)
    PANGAEA
    Details
    Publication Date: 2024-04-18
    Keywords: Acidobacteria, relative 16S rRNA clone frequency; Actinobacteria, relative 16S rRNA clone frequency; alpha-Proteobacteria, relative 16S rRNA clone frequency; Anaerobic methanotrophic archaea-2-a-2b, relative 16S rRNA clone frequency; Anaerobic methanotrophic archaea-2c, relative 16S rRNA clone frequency; Anaerobic methanotrophic archaea-3, relative 16S rRNA clone frequency; ANT06-05 archaea, relative 16S rRNA clone frequency; Bacteria, unaffiliated, relative 16S rRNA clone frequency; Bacteroidetes, relative 16S rRNA clone frequency; beta-Proteobacteria, relative 16S rRNA clone frequency; CCA47 archaea, relative 16S rRNA clone frequency; Chloroflexi, relative 16S rRNA clone frequency; Deep Sea Euryarchaeal Group, relative 16S rRNA clone frequency; Delta-Proteobacteria, relative 16S rRNA clone frequency; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; East of New Zealand, Omakere Ridge; East of New Zealand, Wairarapa Takahae; Epsilon-Proteobacteria, relative 16S rRNA clone frequency; Event label; Fibrobacteres, relative 16S rRNA clone frequency; Gammaproteobacteria, relative 16S rRNA clone frequency; Habitat; Marine Benthic Group A, relative 16S rRNA clone frequency; Marine Benthic Group B, relative 16S rRNA clone frequency; Marine Benthic Group D, relative 16S rRNA clone frequency; Marine Benthic Group E, relative 16S rRNA clone frequency; Marine group I, relative 16S rRNA clone frequency; Methanimicrococcus, relative 16S rRNA clone frequency; Methanococcoides, relative 16S rRNA clone frequency; Methanosalsum, relative 16S rRNA clone frequency; Miscellaneous Crenarchaeotic Group, relative 16S rRNA clone frequency; Multicorer with television; NEW VENTS; Nitrospira, relative 16S rRNA clone frequency; Number of clones; PCR using ARCH20Fb (Massana et al., 1997) and Uni1292R (Lane et al., 1985) prime; PCR using GM3/GM4 primer (Muyzer et al., 1993); Planctomycetes, relative 16S rRNA clone frequency; SO191/2; SO191/2_045; SO191/2_078; SO191/3; SO191/3_309-2; SO191/3_315; Sonne; Thermoplasmatales, relative 16S rRNA clone frequency; TVMUC
    Type: Dataset
    Format: text/tab-separated-values, 93 data points
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    DATA PANGAEA
  • 6
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    Long-Term Evolution of the Martian Crust-Mantle System (2013)
    In:  Space Science Reviews
    Details
    Publication Date: 2020-02-12
    Type: info:eu-repo/semantics/article
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    PAPER (OA)
  • 7
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    Rupture process of the great 1963 Kurile Islands earthquake sequence: Asperity interaction and multiple event rupture (1987)
    In:  J. Geophys. Res., Luxembourg, Conseil de l'Europe, vol. 92, no. 2, pp. 14123-14138, pp. 1892
    Details
    Publication Date: 1987
    Keywords: Earthquake ; Earthquake asperities ; Fracture ; JGR
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    BIBLIOGRAPHY SEISMOLOGY
  • 8
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    Analysis of the trade-off between hypocentral depth and source time function (1985)
    In:  Bull. Seism. Soc. Am., Taipei, Elsevier, vol. 75, no. 3, pp. 1637-1656, pp. RG2001, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1985
    Keywords: Source parameters ; Source ; Seismology ; Hypocentral depth ; BSSA
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    BIBLIOGRAPHY SEISMOLOGY
  • 9
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    Rupture process of the March 3, 1985 Chilean earthquake (1986)
    In:  Geophys. Res. Lett., Taipei, Elsevier, vol. 13, no. 3, pp. 721-724, pp. RG2001, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1986
    Keywords: Earthquake precursor: prediction research ; GRL ; Earthquake ; Source mechanics ; Source parameters
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    BIBLIOGRAPHY SEISMOLOGY
  • 10
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    Seismic coupling and outer rise earthquakes (1988)
    In:  J. Geophys. Res., Taipei, Elsevier, vol. 93, no. 3, pp. 13421-13444, pp. RG2001, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1988
    Keywords: Subduction zone ; Earthquake ; Stress ; Seismicity ; JGR
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    BIBLIOGRAPHY SEISMOLOGY
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