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  • 2000-2004  (9)
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  • 1
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    Unknown
    Schweizerbart Science Publishers
    In:  Neues Jahrbuch für Geologie und Paläontologie - Abhandlungen, 230 . pp. 299-318.
    Publication Date: 2019-02-27
    Type: Article , PeerReviewed
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  • 2
    Publication Date: 2020-04-23
    Description: The Upper Rhine graben is a north-northeast-trending, small-displacement, crustal-scale rift of Tertiary age. Retrodeformation of its southeastern part demonstrates that it is a product of sinistral oblique rifting. Early extension was toward 80°. Later, the major stretching axis changed to a 60° direction. The modeling results suggest that the eastern Main Border fault developed first, and that faulting later propagated into the evolving graben interior. Considerable along-strike variations in heave, throw, and displacement are evident. Displacement partitioning causes warping of the rift floor with a 30-35-km wavelength. We consider this to be a characteristic of oblique rifting. Contact deformation of the wall rocks to the major faults may have caused widespread smaller scale faulting and brecciation and may be the location of later movements. Close spatial coincidence of the depth projections of some of the faults studied and the hypocenters of recent small earthquakes indicates continuing activity of the fault system. Apparently, three fault segments in the Freiburg area are currently active and may be an increased earthquake risk.
    Type: Article , PeerReviewed
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Kopf, Achim J; Behrmann, Jan-Hinrich; Deyhle, Annette; Roller, Sybille; Erlenkeuser, Helmut (2003): Isotopic evidence (B, C, O) of deep fluid processes in fault rock from the active Woodlark Basin detachment zone. Earth and Planetary Science Letters, 208(1-2), 51-68, https://doi.org/10.1016/S0012-821X(03)00016-5
    Publication Date: 2024-01-09
    Description: We report results from boron, carbon and oxygen stable isotope analyses of faulted and veined rocks recovered by scientific ocean drilling during ODP Leg 180 in the western Woodlark Basin, off Papua New Guinea. In this area of active continental extension, crustal break-up and incipient seafloor spreading, a shallow-dipping, seismically active detachment fault accommodates strain, defining a zone of mylonites and cataclasites, vein formation and fluid infiltration. Syntectonic microstructures and vein-fill mineralogy suggest frictional heating during slip during extension and exhumation of Moresby Seamount. Low carbon and oxygen isotope ratios of calcite veins indicate precipitation from hydrothermal fluids (delta13C PDB down to -17 per mil ; delta18O PDB down to -22 per mil ) formed by both dehydration and decarbonation. Boron contents are low (〈7 ppm), indicating high-grade metamorphic source rock for the fluids. Some of the delta11B signatures (17-35 per mil ; parent solutions to calcite vein fills) are low when compared to deep-seated waters in other tectonic environments, likely reflecting preferential loss of 11B during low-grade metamorphism at depth. Pervasive devolatilization and flux of CO2-rich fluids are evident from similar vein cement geochemistry in the detachment fault zone and splays further updip. Multiple rupture-and-healing history of the veins suggests that precipitation may be an important player in fluid pressure evolution and, hence, seismogenic fault movement.
    Keywords: 180-1108; 180-1110; 180-1111; 180-1112; 180-1113; 180-1114; 180-1117; COMPCORE; Composite Core; Joides Resolution; Leg180; Ocean Drilling Program; ODP; Solomon Sea
    Type: Dataset
    Format: application/zip, 5 datasets
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  • 4
    Publication Date: 2024-01-09
    Keywords: 180-1108; Boron; Calculated from stable oxygen isotopes; COMPCORE; Composite Core; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Inductively coupled plasma - mass spectrometry (ICP-MS); Joides Resolution; Leg180; Mass spectrometer Finnigan MAT 251; Ocean Drilling Program; ODP; Sample code/label; Solomon Sea; Temperature, calculated; δ11B; δ13C; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 122 data points
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  • 5
    Publication Date: 2024-01-09
    Keywords: 180-1110; 180-1111; 180-1113; Boron; Calculated from stable oxygen isotopes; COMPCORE; Composite Core; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Event label; Inductively coupled plasma - mass spectrometry (ICP-MS); Joides Resolution; Leg180; Lithology/composition/facies; Mass spectrometer Finnigan MAT 251; Ocean Drilling Program; ODP; Sample code/label; Solomon Sea; Temperature, calculated; δ11B; δ13C; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 29 data points
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  • 6
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    Unknown
    PANGAEA
    In:  Supplement to: Roller, Sybille; Pohl, C; Behrmann, Jan-Hinrich (2003): Data report: Triaxial shear strength of sediments and sedimentary rocks from the Japan Trench, ODP Leg 186. In: Suyehiro, K; Sacks, IS; Acton, GD; Oda, M (eds.) Proceedings of the Ocean Drilling Program, Scientific Results, College Station, TX (Ocean Drilling Program), 186, 1-19, https://doi.org/10.2973/odp.proc.sr.186.115.2003
    Publication Date: 2024-01-09
    Description: In order to determine the shear parameters of the forearc sedimentary strata drilled during Ocean Drilling Program Leg 186, West Pacific Seismic Network, Japan Trench, eight whole-round samples were selected from different depths in the drilled sections of Sites 1150 and 1151. Whereas Site 1150 lays above the seismically active part of the subduction zone, Site 1151 is situated in an aseismic zone. The aim of the triaxial tests was, apart from determination of the static stress strain behavior of the sediments, to test the hypothesis that the static stress strain parameter could differ for each sites. In order to simulate undrained deformation conditions according to the high clay mineral content of the strata, consolidated undrained shear tests were performed in a triaxial testing setup. Measurements of water content, grain density, organic content, and microtextural investigations under the scanning electron microscope (SEM) accompanied the compression experiments. After the saturation and consolidation stages were completed, failure occurred in the compression stage of the experiments at peak strengths of 280-7278 kPa. The stiffness moduli calculated for each sample from differential stress vs. strain curves show a linear relationship with depth and range between 181 and 5827 kPa. Under the SEM, the artificial fault planes of the tested specimen only show partial alignment of clay minerals because of the high content of microfossils.
    Keywords: 186-1150A; 186-1150B; 186-1151A; Calculated from weight loss after ignition at 550 °C; Consolidation stress; Deformation, rate; Density, grain; DEPTH, sediment/rock; Diameter; DRILL; Drilling/drill rig; DSDP/ODP/IODP sample designation; Event label; Height; Induration; Joides Resolution; Leg186; Lithology/composition/facies; Method comment; North Pacific Ocean; Ocean Drilling Program; ODP; Organic matter; Pressure, difference; Pressure, porewater excess; Sample code/label; Sample ID; Scanning electron microscope (SEM); Stiffness modulus; Water content, wet mass
    Type: Dataset
    Format: text/tab-separated-values, 185 data points
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  • 7
    Publication Date: 2024-01-09
    Keywords: 180-1117; Boron; Calculated from stable oxygen isotopes; COMPCORE; Composite Core; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Inductively coupled plasma - mass spectrometry (ICP-MS); Joides Resolution; Leg180; Lithology/composition/facies; Mass spectrometer Finnigan MAT 251; Ocean Drilling Program; ODP; Sample code/label; Solomon Sea; Temperature, calculated; δ11B; δ13C; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 44 data points
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  • 8
    Publication Date: 2024-01-09
    Keywords: 180-1114; Boron; Calculated from stable oxygen isotopes; COMPCORE; Composite Core; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Inductively coupled plasma - mass spectrometry (ICP-MS); Joides Resolution; Leg180; Lithology/composition/facies; Mass spectrometer Finnigan MAT 251; Ocean Drilling Program; ODP; Sample code/label; Solomon Sea; Temperature, calculated; δ11B; δ13C; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 63 data points
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  • 9
    Publication Date: 2024-01-09
    Keywords: 180-1112; Boron; Calculated from stable oxygen isotopes; COMPCORE; Composite Core; DEPTH, sediment/rock; DSDP/ODP/IODP sample designation; Inductively coupled plasma - mass spectrometry (ICP-MS); Joides Resolution; Leg180; Lithology/composition/facies; Mass spectrometer Finnigan MAT 251; Ocean Drilling Program; ODP; Sample code/label; Solomon Sea; Temperature, calculated; δ11B; δ13C; δ18O
    Type: Dataset
    Format: text/tab-separated-values, 41 data points
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