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  • 1
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    PANGAEA
    In:  Supplement to: Wilson, Moyra E J; Hirano, Satoshi; Fergusson, Christopher L; Steurer, Joan; Underwood, Michael B (2003): Data report: Sedimentological and petrographic characteristics of volcanic ashes and siliceous claysontes (altered ashes) from Sites 1173, 1174, and 1177, Leg 190. In: Mikada, H; Moore, GF; Taira, A; Becker, K; Moore, JC; Klaus, A (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 190/196, 1-9, https://doi.org/10.2973/odp.proc.sr.190196.204.2003
    Publication Date: 2024-01-09
    Description: Leg 190 was the first of a two-leg program across the Nankai accretionary prism and Trough, offshore Japan, aiming to evaluate existing models for prism evolution and to constrain syntectonic sedimentation, deformation styles, mechanical properties, and prism hydrology (Moore, Taira, Klaus, et al., 2001; Moore et al., 2001). More than 400 volcanic ash and siliceous claystone (altered ash) layers were penetrated and sampled during drilling of the six sites from two transects across the accretionary prism (Sites 1173-1178). In sites from the subducting Shikoku Basin (Sites 1173 and 1177) and in the trench axis (Site 1174), recognition of ash layers and diagenetically altered ashes was initially important in defining major lithostratigraphic units. However, it is clear that understanding the diagenesis of the volcanic ashes has considerable implications for prism evolution, mechanical properties, prism hydrology, geochemistry, and fluid flow in the accretionary prism and associated subducting sediments (cf. Masuda et al., 1996, doi 10.1346/CCMN.1996.0440402). Particle size, chemical composition, temperature, depth of burial, and time are all thought to be factors that may affect volcanic ash diagenesis and preservation (Kuramoto et al., 1992, doi:10.2973/odp.proc.sr.127128-2.235.1992; Underwood et al., 1993, doi:10.2973/odp.proc.sr.131.137.1993). The overall aim of this research is to evaluate factors influencing volcanic ash diagenesis in the Nankai Trough area. This data report presents just the results of the sedimentological and petrographic analysis of the volcanic ashes and siliceous claystones from Sites 1173, 1174, and 1177. It is anticipated that when the results of additional geochemical analysis of these lithologies is available a more meaningful evaluation of factors influencing volcanic ash alteration will be possible.
    Keywords: 190-1173A; 190-1174A; 190-1174B; 190-1177A; DRILL; Drilling/drill rig; Joides Resolution; Leg190; Ocean Drilling Program; ODP; Philippine Sea
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 2
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    Unknown
    PANGAEA
    In:  Supplement to: Hirano, Satoshi; Ogawa, Yujiro; Kawamura, Kiichiro (2001): Deformation of unlithified sediments in an early stage of the compaction process deduced from microtextures and magnetic fabrics: ODP Leg 174B, Hole 1074A. In: Becker, K; Malone, MJ (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 174B, 1-13, https://doi.org/10.2973/odp.proc.sr.174B.131.2001
    Publication Date: 2024-01-09
    Description: To reveal compaction processes and mechanisms, we have studied microtextures and magnetic fabrics of unlithified sediments collected from Hole 1074A, on the eastern flank of the Mid-Atlantic Ridge, during Leg 174B. Samples consisted of nannofossil ooze with varying amounts of foraminifers, clay, radiolarians and sand. Scanning electron microscope observation shows that nannofossils and planktonic foraminifers in the sediments are well preserved, that void space in the unlithified sediments is formed by an assemblage of microfossils consisting of a stairstep structure of nannofossils and an aggregation of foraminifers, and that the number of spine-shaped nannofossil fragments tends to increase with depth, suggesting weak deformation probably due to compaction occurring during burial. Anisotropy of magnetic susceptibility results, however, provide little obvious information about deformation of the sediments. These results are consistent with those of the onboard multisensor track measurements.
    Keywords: 174-1074A; Anisotropy-magnetic susceptibility, factor F, foliation; Anisotropy-magnetic susceptibility, factor L, lineation; Congo Fan, Angola Basin, North Atlantic Ocean; DEPTH, sediment/rock; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Inclination of principle axis K1; Inclination of principle axis K3; Joides Resolution; Kappabridge, AGICO KLY-3S; Leg174B; Magnetic susceptibility, volume; Ocean Drilling Program; ODP; Sample code/label
    Type: Dataset
    Format: text/tab-separated-values, 667 data points
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  • 3
    Publication Date: 2024-01-09
    Keywords: 190-1173A; Biotite; Carbonates; Clay; Clay minerals; Color description; Depth, bottom/max; Depth, reference; DEPTH, sediment/rock; Depth, top/min; Description; Diatom abundance; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Epoch; Feldspar; Foraminifera; Grain size description; Igneous rock; Joides Resolution; Leg190; Lithic grains; Lithologic unit/sequence; Lithology/composition/facies; Minerals; Muscovite; Nannofossil abundance; Nannofossil zone; Ocean Drilling Program; ODP; Opaque minerals; Philippine Sea; Pyrite; Quartz; Radiolarians abundance; Sample code/label; Sample comment; Sample thickness; Sand; Section; Section position; Silicoflagellate abundance; Silt; Smear slide analysis; Sorting description; Sponge spiculae; Volcanic glass; Volcanic glass, altered; Zeolite
    Type: Dataset
    Format: text/tab-separated-values, 4035 data points
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  • 4
    Publication Date: 2024-01-09
    Keywords: 190-1174A; 190-1174B; Biotite; Carbonates; Clay; Clay minerals; Color description; Depth, bottom/max; Depth, reference; DEPTH, sediment/rock; Depth, top/min; Description; Diatom abundance; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Epoch; Event label; Feldspar; Foraminifera; Grain size description; Joides Resolution; Leg190; Lithic grains; Lithologic unit/sequence; Lithology/composition/facies; Mica; Minerals; Nannofossil abundance; Nannofossil zone; Ocean Drilling Program; ODP; Opaque minerals; Philippine Sea; Quartz; Radiolarians abundance; Sample code/label; Sample comment; Sample thickness; Sand; Section; Section position; Silt; Smear slide analysis; Sorting description; Volcanic glass; Volcanic glass, altered; Zeolite
    Type: Dataset
    Format: text/tab-separated-values, 3363 data points
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  • 5
    Publication Date: 2024-01-09
    Keywords: 190-1177A; Carbonates; Clay; Clay minerals; Color description; Depth, bottom/max; Depth, reference; DEPTH, sediment/rock; Depth, top/min; Description; Diatom abundance; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Epoch; Feldspar; Foraminifera; Grain size description; Joides Resolution; Leg190; Lithic grains; Lithologic unit/sequence; Lithology/composition/facies; Mica; Minerals; Nannofossil abundance; Nannofossil zone; Ocean Drilling Program; ODP; Opaque minerals; Organic matter; Philippine Sea; Quartz; Radiolarians abundance; Sample code/label; Sample comment; Sample thickness; Sand; Section; Section position; Silt; Smear slide analysis; Sorting description; Volcanic glass; Volcanic glass, altered; Zeolite
    Type: Dataset
    Format: text/tab-separated-values, 1385 data points
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  • 6
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Journal of Applied Physics 87 (2000), S. 6552-6554 
    ISSN: 1089-7550
    Source: AIP Digital Archive
    Topics: Physics
    Notes: A fast numerical method is developed in which the LaBonte method is accelerated using one of the multigrid methods, the V-cycle method. The developed method is based on the previously derived equilibrium equation which has a form amenable to implementation in the multigrid schemes. The basic property of the derived method is presented together with a summary of derivation and the results of calculations which demonstrate the effectiveness of the method. © 2000 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 7
    Electronic Resource
    Electronic Resource
    [S.l.] : American Institute of Physics (AIP)
    Journal of Applied Physics 85 (1999), S. 6205-6207 
    ISSN: 1089-7550
    Source: AIP Digital Archive
    Topics: Physics
    Notes: A numerical scheme is presented in which a static micromagnetic calculation is performed using one of the multigrid methods, the V-cycle method. An equilibrium equation in which the discretized Laplacian of magnetization is solved is derived from the magnetic energy and relaxed in the V-cycle method based on the weighted Jacobi relaxation. Calculations made for a one-dimension Bloch wall and a flux-closure structure in Permalloy™ films show the validity and the versatility of the new scheme. © 1999 American Institute of Physics.
    Type of Medium: Electronic Resource
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  • 8
    ISSN: 1440-1738
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract A 1800 m deep borehole was drilled at Nojima Hirabayashi, Japan to penetrate through the Nojima Fault, which was activated at the time of the 1995 Hyogo-ken Nanbu earthquake (Kobe earthquake). Three fracture zones were recognized in cores at approximate depths of 1140 m, 1300 m and 1800 m. The mode of distribution of fault rocks, minerals and chemical elements were analyzed in an interval between depths of 1108 m and 1161 m, focusing on the fracture zone at the depth of 1140 m. Foliated blue-gray fault gouge constituted the central part of the fracture zone. The degree of fracturing appeared to be greater in the hanging wall than in the footwall. The relative amounts of minerals were estimated qualitatively. In the analyzed interval, not only were quartz, orthoclase, plagioclase, biotite and hornblende detected in the parent rock (granodiorite), but also kaolinite, smectite, laumontite, stilbite, calcite, ankerite and siderite, which are related to hydrothermal alteration. In particular, biotite disappeared both in the hanging wall and footwall across the central fault zone; it disappeared over a wider range in the hanging wall than in the footwall. The amounts of major chemical elements were analyzed quantitatively. Concentrations of Al2O3, Fe2O3, MnO, TiO2, and P2O5 all decreased throughout the interval except at some points. H2O+ and CO2 increased throughout the interval. Na2O increased in the region outside the central plane, whereas MgO and CaO increased in the hanging wall and decreased in the footwall. SiO2 and K2O decreased in the hanging wall and increased in the footwall. These results elucidate the higher degree of fracturing and chemical changes present in the hanging wall of the 1140 m fracture zone than in the footwall.
    Type of Medium: Electronic Resource
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  • 9
    ISSN: 1440-1738
    Source: Blackwell Publishing Journal Backfiles 1879-2005
    Topics: Geosciences
    Notes: Abstract Characteristics of deformation and alteration of the 1140 m deep fracture zone of the Nojima Fault are described based on mesoscopic (to the naked eye) and microscopic (by both optical and scanning electron microscopes) observations of the Hirabayashi National Research Institute for Earth Science and Disaster Prevention (NIED) drill core. Three types of fault rocks; that is, fault breccia, fault gouge and cataclasite, appear in the central part of the fault zone and two types of weakly deformed and/or altered rocks; that is, weakly deformed and altered granodiorite and altered granodiorite, are located in the outside of the central part of the fault zone (damaged zone). Cataclasite appears occasionally in the damaged zone. Six distinct, thin foliated fault gouge zones, which dip to the south-east, appear clearly in the very central part of the fracture zone. Slickenlines plunging to the north-east are observed on the surface of the newest gouge. Based on the observations of XZ thin sections, these slickenlines and the newest gouge have the same kinematics as the 1995 Hyogo-ken Nanbu earthquake (Kobe earthquake), which was dextral-reverse slip. Scanning electron microscopy observations of the freeze-dried fault gouge show that a large amount of void space is maintained locally, which might play an important role as a path for fluid migration and the existence of either heterogeneity of pore fluid pressure or strain localization.
    Type of Medium: Electronic Resource
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  • 10
    Electronic Resource
    Electronic Resource
    [s.l.] : Nature Publishing Group
    Nature structural & molecular biology 13 (2006), S. 272-277 
    ISSN: 1545-9985
    Source: Nature Archives 1869 - 2009
    Topics: Biology , Medicine
    Notes: [Auszug] Hrs has an essential role in sorting of monoubiquitinated receptors to multivesicular bodies for lysosomal degradation, through recognition of ubiquitinated receptors by its ubiquitin-interacting motif (UIM). Here, we present the structure of a complex of Hrs-UIM and ubiquitin at 1.7-Å ...
    Type of Medium: Electronic Resource
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