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  • 1
    Monograph available for loan
    Monograph available for loan
    Photographic atlas of an accretionary prism : geologic structures of the Shimanto Belt, Japan (1992)
    Berlin [u.a.] : Springer-Verl.
    Details Availability
    Call number: M 92.0793
    Type of Medium: Monograph available for loan
    Pages: 124 S. : farb. Abb.
    ISBN: 3540553444
    Classification:
    Regional Geology
    Language: English
    Location: Upper compact magazine
    Branch Library: GFZ Library
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  • 2
    Electronic Resource
    Electronic Resource
    Kinetics of degenerate rearrangements in nortricyclyl cation (1988)
    s.l. : American Chemical Society
    Journal of the American Chemical Society 110 (1988), S. 8287-8291 
    Details
    ISSN: 1520-5126
    Source: ACS Legacy Archives
    Topics: Chemistry and Pharmacology
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1021/ja00233a002
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    Paper (German National Licenses)
    Fulltext
  • 3
    Electronic Resource
    Electronic Resource
    Broad analysis reveals a consistent pattern of var gene transcription in Plasmodium falciparum repeatedly selected for a defined adhesion phenotype (2005)
    Oxford, UK : Blackwell Science Ltd
    Molecular microbiology 56 (2005), S. 0 
    Details
    ISSN: 1365-2958
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Biology , Medicine
    Notes: Transcription of the majority of the members of the Plasmodium falciparum var multigene family were analysed in two isolates by a quantitative approach. Both of these isolates had been repeatedly selected for adhesion to chondroitin sulphate A (CSA) and one had also been selected for adhesion to hyaluronic acid (HA). These adhesion phenotypes are expressed by many parasites isolated from placentae and are associated with malaria disease in pregnancy. Increased transcription of the var gene var2csa, or its homologue IT4 var4, was associated with the CSA and HA adhesion phenotypes in all parasites suggesting that it was the dominant, if not the only, var gene that encoded adhesion to CSA in these allogeneic isolates. Some var genes were consistently transcribed at higher levels than others regardless of expressed adhesion phenotypes suggesting a transcriptional hierarchy. Unspliced or partial transcripts were detected for most var genes tested. These atypical var gene transcripts may have implications for the regulation of var gene transcription.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1365-2958.2005.04577.x
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  • 4
    Electronic Resource
    Electronic Resource
    Sensitivity of Cultured Skin Fibroblasts from Patients with Neurofibromatosis to DNA-Damaging Agents (1986)
    Oxford, UK : Blackwell Publishing Ltd
    Annals of the New York Academy of Sciences 486 (1986), S. 0 
    Details
    ISSN: 1749-6632
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Natural Sciences in General
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1111/j.1749-6632.1986.tb48087.x
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  • 5
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    (Table 2) CT scan measurements of ODP Site 131-808 (1993)
    PANGAEA
    In:  Supplement to: Soh, Wonn; Byrne, Timothy; Taira, Asahiko; Kono, Atsushi (1993): Computed tomography (CT) scan image analysis of Site 808 cores: structural and physical property implications. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 135-140, https://doi.org/10.2973/odp.proc.sr.131.113.1993
    Details
    Publication Date: 2024-01-09
    Description: X-ray computed tomography (CT) is a promising tool that yields data useful for understanding the fine-scale density structure of partly lithified and tectonically deformed sediments. We conducted 21 CT scans of ODP Leg 131 sediments, including whole-round cores and thin-section chips, obtained from the toe of the Nankai accretionary prism. The samples range from highly deformed pieces from the frontal thrust and décollement to homogeneous and essentially undeformed sediments above the frontal thrust and beneath the décollement. In the CT images, kink-like deformation bands and faults are recognized as obvious bright seams, bands, or stripes with relatively high linear attenuation coefficients. The differences in linear attenuation coefficients relative to the matrix range from 0.021 cm**2/g (kink-like deformation band) to 0.038 cm**2/g (fault). These data suggest a 0.10 g/cm**3 to 0.18 g/cm**3 increase in bulk density within the deformation structures, and they appear to be 13% and 33% more compacted than the nondeformed matrix, respectively. In contrast to the samples from the frontal thrust zone, CT images of the décollement sample exhibit relatively homogeneous textures. The attenuation coefficient of the sample of the décollement indicates bulk density and porosity values of 2.45 g/cm**3 and 18%, respectively. The sample, hence, is approximately 50% more compacted than the sediment outside the décollement zone.
    Keywords: 131-808; Attenuation value; Attenuation value, standard deviation; COMPCORE; Composite Core; Density, wet bulk; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Joides Resolution; Leg131; Ocean Drilling Program; ODP; Philippine Sea; Porosity; Sample code/label; Sample comment; X-ray computed tomography (CT)
    Type: Dataset
    Format: text/tab-separated-values, 116 data points
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  • 6
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    (Table 1) Summary of CT values, attenuation coefficients, density, and porosity of ODP Site 131-808A samples (1993)
    PANGAEA
    In:  Supplement to: Byrne, Timothy; Maltman, Alex J; Stephenson, Emma; Soh, Wonn; Knipe, Rob (1993): Deformation structures and fluid flow in the toe region of the Nankai accretionary prism. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 83-101, https://doi.org/10.2973/odp.proc.sr.131.107.1993
    Details
    Publication Date: 2024-01-09
    Description: This paper presents results of an interdisciplinary investigation of the relation between fluids, fluid flow, and deformation in the toe region of the Nankai accretionary prism. The techniques include thin-section petrography, SEM, TEM and microprobe analyses, and X-ray computed tomography as well as laboratory experiments. Together, the data suggest three structural/hydrologic regimes within the prism. These are: (1) the accreting sediments above the décollement zone, (2) the décollement zone, and (3) the underthrust sediments. The regime above the décollement is characterized by sediments that are progressively dewatered through both a penetrative fabric and a pervasive, but apparently poorly interconnected, set of core-scale deformation structures. The décollement is characterized by a relatively high density of structures/meter and is considered to be a regime of low stress but frequent failure. Hydrologically the décollement retards the vertical flow of fluids and enhances the potential for overpressuring in the footwall. Finally, the footwall regime contains very few tectonic structures and is structurally isolated from the stresses related to plate convergence. This regime provides an important component to the tectonics of the Nankai prism, however, because it supplies the overpressured fluids that cause the d?collement to fail at relatively low shear stresses.
    Keywords: 131-808; Attenuation value; COMPCORE; Composite Core; Computer tomograph value; Density; DEPTH, sediment/rock; Difference; DSDP/ODP/IODP sample designation; Joides Resolution; Leg131; Number; Ocean Drilling Program; ODP; Philippine Sea; Porosity; Sample code/label; Water content, wet mass; X-ray computed tomography (CT)
    Type: Dataset
    Format: text/tab-separated-values, 161 data points
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  • 7
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    (Table 3) Main results of the stress tensor inversion of selected populations of slickenlined faults at OPD Hole 131-808C (1993)
    PANGAEA
    In:  Supplement to: Lallemant, Siegfried J; Byrne, Timothy; Maltman, Alex J; Karig, Daniel E; Henry, Pierre (1993): Stress tensors at the toe of the Nankai accretionary prism: an application of inverse methods to slickenlined faults. In: Hill, IA; Taira, A; Firth, JV; et al. (eds.), Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 131, 103-122, https://doi.org/10.2973/odp.proc.sr.131.109.1993
    Details
    Publication Date: 2024-01-09
    Description: Drilling at Site 808 (ODP Leg 131) provided an extensive record of the discrete brittle structures (small faults and shear bands) at the toe of the Nankai accretionary complex. Brittle failure is occurring throughout the hole, although most of the deformation has been observed between the frontal thrust and the décollement (from 365 to 963 mbsf). Brittle failure occurs in the turbiditic trench fill (0 to 600 mbsf) but also in the ash-bearing hemipelagites from the upper Shikoku Basin (600 to 800 mbsf) and the ash-free hemipelagites of the lower Shikoku Basin sequences, down to the décollement (963 mbsf). The geometry of the tectonic features has been recorded in a local frame related to the core liner and then corrected to an absolute frame by the use of paleomagnetic measurements. We used the resulting geometry of homogeneous populations of slickenlined faults to estimate the reduced stress tensor. The main result is to show three consistent stress patterns. Most of the fault clusters from the frontal thrust down to the décollement are in good agreement with a compressional regime with a northwest-trending sigma 1 (azimuth N305° to N315°). The compression direction is thus roughly parallel to the local direction of the relative convergence. It is also perpendicular to the trend of the anticlinal ridges. Discrete faults, locally appearing as clusters (e.g., 30 m above the décollement) agree with a quite different compression direction (west-southwest-east-northeast) and are restricted to the hemipelagic sequences above the décollement. They could be related to the heterogeneous internal deformation of this layer. Although isolated normal faults exist, their occurrence as clusters is restricted to the Shikoku Basin hemipelagic sequences and indicate a east-west to northwest-southeast extension axis (?3). Finally, the analysis of Mohr diagrams related to the best-fitting tensors shows some similarities and differences between the fault populations of the turbidite and those of the hemipelagite sequences. The angle of friction corresponding to 95% of the data is 30° +/- 5°, whereas including the remaining 5% in turbidites and hemipelagites would result in a lower friction angle (18° +/- 8°). The major difference concerns the angle between conjugate sets which are about 60° in the turbidites and lower (35°- 40°) in a 200 m thick zone above the décollement and can be explained by higher fluid pressure in the hemipelagites or by odd mechanical properties of this hemipelagic material.
    Keywords: 131-808C; Angle; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Joides Resolution; Leg131; Number of faults; Ocean Drilling Program; ODP; Philippine Sea; Plunge; Ratio; Sample code/label; Sample code/label 2; Trend
    Type: Dataset
    Format: text/tab-separated-values, 173 data points
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  • 8
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    Core-section summary from IODP Hole 319-C0009A (2012)
    PANGAEA
    In:  SIO7 Data Center, J-CORES Database; Ocean Drilling Program, Center for Deep Earth Exploration (JAMSTEC)
    Details
    Publication Date: 2024-02-10
    Keywords: 319-C0009A; Chikyu; Core section, comment; Curated Length; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Exp319; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; NanTroSEIZE Stage 2: Riser/Riserless Observatory 1; Sample code/label; Section Bot in meters below surface; Section Top in meters below surface
    Type: Dataset
    Format: text/tab-separated-values, 384 data points
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  • 9
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    Description of lithologic units (VCD) from IODP Hole 319-C0009A (2012)
    PANGAEA
    In:  SIO7 Data Center, J-CORES Database; Ocean Drilling Program, Center for Deep Earth Exploration (JAMSTEC)
    Details
    Publication Date: 2024-02-10
    Keywords: 319-C0009A; Chikyu; Comment; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Exp319; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Main Lithology; NanTroSEIZE Stage 2: Riser/Riserless Observatory 1; Rock type; Sample code/label; Sample code/label 2; Time Stamp; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 6528 data points
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  • 10
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    Distribution of lithologic units from IODP Hole 319-C0009A (2012)
    PANGAEA
    In:  SIO7 Data Center, J-CORES Database; Ocean Drilling Program, Center for Deep Earth Exploration (JAMSTEC)
    Details
    Publication Date: 2024-02-10
    Keywords: 319-C0009A; Chikyu; Comment; Depth, bottom/max; DEPTH, sediment/rock; Depth, top/min; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Exp319; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Main Lithology; NanTroSEIZE Stage 2: Riser/Riserless Observatory 1; Rock type; Sample code/label; Sample code/label 2; Time Stamp; Visual description
    Type: Dataset
    Format: text/tab-separated-values, 6528 data points
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