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  • 2015-2019  (24)
  • 1990-1994
  • 2015  (24)
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  • 2015-2019  (24)
  • 1990-1994
Year
  • 1
    In: Expedition Erde, Bremen : MARUM - Zentrum für Marine Umweltwissenschaften, 2015, (2015), Seite 90-99, 9783000490453
    In: year:2015
    In: pages:90-99
    Type of Medium: Article
    Pages: Ill., graph. Darst.
    Language: German
    Location Call Number Limitation Availability
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  • 2
    In: Expedition Erde, Bremen : MARUM - Zentrum für Marine Umweltwissenschaften, 2015, (2015), Seite 150-157, 9783000490453
    In: year:2015
    In: pages:150-157
    Type of Medium: Article
    Pages: Ill., graph. Darst.
    Language: German
    Location Call Number Limitation Availability
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  • 3
    In: Expedition Erde, Bremen : MARUM - Zentrum für Marine Umweltwissenschaften, 2015, (2015), Seite 86-89, 9783000490453
    In: year:2015
    In: pages:86-89
    Type of Medium: Article
    Pages: Ill., graph. Darst.
    Language: German
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2015-09-24
    Description: Highlights: • Comprehensive morphological, seismic, sedimentological, and geotechnical data sets. • Dynamic CPTU provides a powerful, time- and cost-efficient in situ technique. • Development of a regional sub-seafloor strength model offshore Nice airport. • 2D finite element slope stability assessment gives slope failure depth of 〉 50 m. Abstract: In the landslide-prone area near the Nice international airport, southeastern France, an interdisciplinary approach is applied to develop realistic lithological/geometrical profiles and geotechnical/strength sub-seafloor models. Such models are indispensable for slope stability assessments using limit equilibrium or finite element methods. Regression analyses, based on the undrained shear strength (su) of intact gassy sediments are used to generate a sub-seafloor strength model based on 37 short dynamic and eight long static piezocone penetration tests, and laboratory experiments on one Calypso piston and 10 gravity cores. Significant strength variations were detected when comparing measurements from the shelf and the shelf break, with a significant drop in su to 5.5 kPa being interpreted as a weak zone at a depth between 6.5 and 8.5 m below seafloor (mbsf). Here, a 10% reduction of the in situ total unit weight compared to the surrounding sediments is found to coincide with coarse-grained layers that turn into a weak zone and detachment plane for former and present-day gravitational, retrogressive slide events, as seen in 2D chirp profiles. The combination of high-resolution chirp profiles and comprehensive geotechnical information allows us to compute enhanced 2D finite element slope stability analysis with undrained sediment response compared to previous 2D numerical and 3D limit equilibrium assessments. Those models suggest that significant portions (detachment planes at 20 m or even 55 mbsf) of the Quaternary delta and slope apron deposits may be mobilized. Given that factors of safety are equal or less than 1 when further considering the effect of free gas, a high risk for a landslide event of considerable size off Nice international airport is identified.
    Type: Article , PeerReviewed
    Format: text
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  • 5
    Publication Date: 2023-03-09
    Keywords: Center for Marine Environmental Sciences; Comment; Density, dry bulk; DEPTH, sediment/rock; Elevation of event; Event label; GC; GeoB13919; GeoB13928; GeoB13929; GeoB13936; GeoB13941; GeoB13946; GeoB13952; GeoB16542-1; Gravity corer; Latitude of event; Lithology/composition/facies; Location; Longitude of event; MARUM; Nice Slope; POS386; POS429; POS429_085-1; Poseidon; Sand; Size fraction 〈 0.002 mm, clay; Size fraction 〉 0.006 mm, silt; Size fraction 0.125-0.063 mm, 3.0-4.0 phi, very fine sand; Size fraction 0.250-0.125 mm, 2.0-3.0 phi, fine sand; Size fraction 0.500-0.250 mm, 1.0-2.0 phi, medium sand; Size fraction 2.000-0.630 mm, coarse sand; Size fraction 2.000-1.000 mm, (-1.0)-0.0 phi, very coarse sand; Vertical stress
    Type: Dataset
    Format: text/tab-separated-values, 119 data points
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  • 6
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    PANGAEA
    In:  Supplement to: Stegmann, Sylvia; Kopf, Achim J (2014): How stable is the Nice slope? An analysis based on strength and cohesion from ring shear experiments. In: Krastel S et al. (eds.) Submarine Mass Movements and Their Consequences. Springer, Heidelberg, 189-200, https://doi.org/10.1007/978-3-319-00972-8_17
    Publication Date: 2023-03-03
    Description: The upper shelf of the landslide-prone Ligurian Margin (Western Mediterranean Sea) off Nice well-known for the 1979 Airport Landslide is a natural laboratory to study preconditioning factors and trigger mechanisms for submarine landslides. For this study low-stress ring shear experiments have been carried out on a variety of sediments from 〉50 gravity cores to characterise the velocity-dependent frictional behaviour. Mean values of the peak coefficient of friction vary from 0.46 for clay-dominated samples (53 % clay, 46 % silt, 1 %) sand up to 0.76 for coarse-grained sediments (26 % clay, 57 % silt, 17 % sand). The majority of the sediments tested show velocity strengthening regardless of the grain size distribution. For clayey sediments the peak and residual cohesive strength increases with increasing normal stress, with values from 1.3 to 10.6 kPa and up to 25 % of all strength supported by cohesive forces in the shallowmost samples. A pseudo-static slope stability analysis reveals that the different lithologies (even clay-rich material with clay content 〉=50 %) tested are stable up to slope angles 〈26° under quasi-drained conditions.
    Keywords: Center for Marine Environmental Sciences; MARUM
    Type: Dataset
    Format: application/zip, 2 datasets
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  • 7
    Publication Date: 2023-03-03
    Keywords: Center for Marine Environmental Sciences; Cohesion; Cohesive friction; DEPTH, sediment/rock; Elevation of event; Event label; Friction coefficient; GC; GeoB13919; GeoB13928; GeoB13929; GeoB13936; GeoB13941; GeoB13946; GeoB13952; GeoB16542-1; Gravity corer; Latitude of event; Location; Longitude of event; MARUM; Nice Slope; POS386; POS429; POS429_085-1; Poseidon; Shear behaviour; Shear strength
    Type: Dataset
    Format: text/tab-separated-values, 268 data points
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  • 8
    Publication Date: 2024-02-10
    Keywords: 343-C0019E; Chikyu; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Effective stress; Exp343; Experiment; Friction coefficient; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Japan Trench Fast Drilling Project; Sample code/label; Sample comment; Smectite
    Type: Dataset
    Format: text/tab-separated-values, 196 data points
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  • 9
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    In:  Supplement to: Ikari, Matt J; Kameda, Jun; Saffer, Demian M; Kopf, Achim J (2015): Strength characteristics of Japan Trench borehole samples in the high-slip region of the 2011 Tohoku-Oki earthquake. Earth and Planetary Science Letters, 412, 35-41, https://doi.org/10.1016/j.epsl.2014.12.014
    Publication Date: 2024-02-10
    Description: The 2011 Tohoku-Oki earthquake demonstrated that the shallowest reaches of plate boundary subduction megathrusts can host substantial coseismic slip that generates large and destructive tsunamis, contrary to the common assumption that the frictional properties of unconsolidated clay-rich sediments at depths less than View the MathML source should inhibit rupture. We report on laboratory shearing experiments at low sliding velocities (View the MathML source) using borehole samples recovered during IODP Expedition 343 (JFAST), spanning the plate-boundary décollement within the region of large coseismic slip during the Tohoku earthquake. We show that at sub-seismic slip rates the fault is weak (sliding friction µs=0.2-0.26), in contrast to the much stronger wall rocks (µs〉~0.5). The fault is weak due to elevated smectite clay content and is frictionally similar to a pelagic clay layer of similar composition. The higher cohesion of intact wall rock samples coupled with their higher amorphous silica content suggests that the wall rock is stronger due to diagenetic cementation and low clay content. Our measurements also show that the strongly developed in-situ fabric in the fault zone does not contribute to its frictional weakness, but does lead to a near-cohesionless fault zone, which may facilitate rupture propagation by reducing shear strength and surface energy at the tip of the rupture front. We suggest that the shallow rupture and large coseismic slip during the 2011 Tohoku earthquake was facilitated by a weak and cohesionless fault combined with strong wall rocks that drive localized deformation within a narrow zone.
    Keywords: Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP
    Type: Dataset
    Format: application/zip, 4 datasets
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  • 10
    Publication Date: 2024-02-10
    Keywords: 343-C0019E; Analytical method; Chikyu; Comment; Date; DEPTH, sediment/rock; DRILL; Drilling/drill rig; Effective stress; Exp343; Experiment; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; Japan Trench Fast Drilling Project; Method comment; Sample code/label; Sample comment; Single-direct shear apparatus
    Type: Dataset
    Format: text/tab-separated-values, 439 data points
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