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  • 1
    Keywords: Forschungsreise
    Description / Table of Contents: The research cruise to the Eastern Mediterranean (GPF-18-2-40) originally planned on RV METEOR was relocated to RV SONNE (Fig. 1.2) due to the reduced number of scientists as part of the corona pandemic. The main objective of the Bremen Ocean Cluster expedition (DFG, EXC2077) was to investigate the interactions between the seabed and ocean water in Greek waters, whereby the plate tectonic constellation of a broad collision zone represents a special tectonic drive. A secondary goal was the sampling of the Sartori mud volcano, which is being processed in Italian waters as part of a separate DFG project and for which the GPF granted an additional permit for ship time (GPF 20-1_054). The expedition began on 12 October in Emden/Germany and ended on 01 December 2020, in Emden. Investigations on mud volcanoes were carried out divided into 3 working areas (Fig. 1.1, the Sartori mud volcano in the Calabrian arc, the so-called Cobblestone Area, the Olimpi mud volcano field including the United Nation Ridge). With the MARUM AUV SEAL (Fig. 1.3) 11 dives were successfully carried out to create high-resolution detailed maps of certain seafloor structures. A total of 38 gravity cores (Fig. 1.4), 30 multicorers (Fig. 1.5) and 4 minicorers were used for sampling sediments and 6 CTD stations for sampling methane in the water column. Furthermore, 10 profiles were carried out with the heat flow lance and 5 observation profiles with the on-board OFOS. In four different provinces, 16 mud volcanoes were examined, 10 of which are characterized by pore waters that show a distinct freshening, while three mud volcanoes, Napoli, Heraklion and Gelendzhik, are characterized by very high salt concentrations. The salt accumulations in these structures are derived from the Messinian salt deposits in the subbed, from which salty brines arise through subrosion, which interact in various ways with the mud volcanoes. The study areas were selected based on preliminary surveys and morphological structures and increased backscatter patterns from multibeam mapping carried out over 3580 nautical miles in Italian and Greek waters.
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (208 Seiten)
    Series Statement: Berichte aus dem MARUM und dem Fachbereich Geowissenschaften der Universität Bremen No. 326
    DDC: 551.23
    Language: English
    Location Call Number Limitation Availability
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  • 2
    Description / Table of Contents: The research cruise to the Eastern Mediterranean (GPF-18-2-40) originally planned on RV METEOR was relocated to RV SONNE (Fig. 1.2) due to the reduced number of scientists as part of the corona pandemic. The main objective of the Bremen Ocean Cluster expedition (DFG, EXC2077) was to investigate the interactions between the seabed and ocean water in Greek waters, whereby the plate tectonic constellation of a broad collision zone represents a special tectonic drive. A secondary goal was the sampling of the Sartori mud volcano, which is being processed in Italian waters as part of a separate DFG project and for which the GPF granted an additional permit for ship time (GPF 20-1_054). The expedition began on 12 October in Emden/Germany and ended on 01 December 2020, in Emden. Investigations on mud volcanoes were carried out divided into 3 working areas (Fig. 1.1, the Sartori mud volcano in the Calabrian arc, the so-called Cobblestone Area, the Olimpi mud volcano field including the United Nation Ridge). With the MARUM AUV SEAL (Fig. 1.3) 11 dives were successfully carried out to create high-resolution detailed maps of certain seafloor structures. A total of 38 gravity cores (Fig. 1.4), 30 multicorers (Fig. 1.5) and 4 minicorers were used for sampling sediments and 6 CTD stations for sampling methane in the water column. Furthermore, 10 profiles were carried out with the heat flow lance and 5 observation profiles with the on-board OFOS. In four different provinces, 16 mud volcanoes were examined, 10 of which are characterized by pore waters that show a distinct freshening, while three mud volcanoes, Napoli, Heraklion and Gelendzhik, are characterized by very high salt concentrations. The salt accumulations in these structures are derived from the Messinian salt deposits in the subbed, from which salty brines arise through subrosion, which interact in various ways with the mud volcanoes. The study areas were selected based on preliminary surveys and morphological structures and increased backscatter patterns from multibeam mapping carried out over 3580 nautical miles in Italian and Greek waters.
    Type of Medium: Book
    Pages: 208 Seiten , Illustrationen, Diagramme, Karten
    Series Statement: Berichte aus dem MARUM und dem Fachbereich Geowissenschaften der Universität Bremen No. 326
    Language: English
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  • 3
    Publication Date: 2023-02-24
    Keywords: Comment; Duration; earthquake; Experiment; friction; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; IODP Expedition 375; Machine stiffness; Number; Ratio; Slip; slow slip; Stress drop; Time in hours; Time in seconds; Velocity
    Type: Dataset
    Format: text/tab-separated-values, 5246 data points
    Location Call Number Limitation Availability
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  • 4
    Publication Date: 2024-02-05
    Description: The northern Hikurangi subduction margin hosts slow slip events (SSEs), which are exceptionally shallow (〈15 km). The sedimentary sequence on the incoming plate is therefore representative of the shallow fault material where the SSEs will take place once they enter the subduction zone. Knowledge about the frictional behavior of these sediments is required to know which lithologies are capable of hosting SSEs, and what mechanisms are causing them. Frictional behavior is material-specific and depends on sliding velocity, but it is unknown how these natural sediments behave at plate-rate velocities. We performed laboratory shearing experiments testing the major lithologies sampled during IODP Expedition 375, at velocities ranging from the plate convergence rate at the Hikurangi margin (5 cm/year), up to those characteristic of the shallow SSEs (160 and 530 cm/year), under simulated in-situ as well as standardized conditions. We observe spontaneous laboratory SSEs in the calcareous pelagic sediments, which show partial locking in between sliding events consistent with the interpretation of SSEs within the spectrum of slow to fast earthquakes. This dataset includes the frictional parameters needed to assess the frictional stability of the tested materials, as well as details about the laboratory slip events.
    Keywords: earthquake; friction; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; IODP Expedition 375; slow slip
    Type: Dataset
    Format: application/zip, 3 datasets
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-02-10
    Keywords: 375-U1520C; 375-U1520D; CDRILL; Comment; Core drilling; Critical slip distance dc1; Critical slip distance dc1, standard deviation; Critical slip distance dc2; Critical slip distance dc2, standard deviation; Critical stiffness kc; Critical stiffness kc, normalized; Description; earthquake; Event label; Exp375; Experiment; friction; Friction coefficient; Friction direct effect; Friction direct effect, standard deviation; Friction evolutionary effect, b1; Friction evolutionary effect, b2; Friction evolutionary effect b1, standard deviation; Friction evolutionary effect b2, standard deviation; Initial friction coefficient; Initial friction coefficient, standard deviation; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; IODP Expedition 375; Joides Resolution; Linear detrending; Machine stiffness; Machine stiffness, standard deviation; Sample code/label; Sliding velocity, final; Sliding velocity, initial; slow slip; Steady-state friction coefficients; Velocity-dependent friction parameter; Velocity-dependent friction parameter, standard deviation; Weight function
    Type: Dataset
    Format: text/tab-separated-values, 876 data points
    Location Call Number Limitation Availability
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  • 6
    Publication Date: 2024-02-10
    Keywords: 375-U1520C; 375-U1520D; CDRILL; Comment; Core drilling; Critical slip distance dc1; Critical slip distance dc1, standard deviation; Critical slip distance dc2; Critical slip distance dc2, standard deviation; Critical stiffness kc; Critical stiffness kc, normalized; DEPTH, sediment/rock; Description; earthquake; Event label; Exp375; Experiment; friction; Friction coefficient; Friction direct effect; Friction direct effect, standard deviation; Friction evolutionary effect, b1; Friction evolutionary effect, b2; Friction evolutionary effect b1, standard deviation; Friction evolutionary effect b2, standard deviation; Initial friction coefficient; Initial friction coefficient, standard deviation; Integrated Ocean Drilling Program / International Ocean Discovery Program; IODP; IODP Expedition 375; Joides Resolution; Linear detrending; Machine stiffness; Machine stiffness, standard deviation; Normal stress; Sample code/label; Sample type; Sliding velocity, final; Sliding velocity, initial; slow slip; Steady-state friction coefficients; Velocity-dependent friction parameter; Velocity-dependent friction parameter, standard deviation; Weight function
    Type: Dataset
    Format: text/tab-separated-values, 466 data points
    Location Call Number Limitation Availability
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  • 7
    Publication Date: 2024-03-22
    Description: The potential of faults to show earthquake-generating slip instabilities depends not only on the intrinsic frictional properties of the fault zone, but also on the elasticity of the surrounding material. A velocity-weakening fault is expected to show increasingly unstable frictional behavior with decreasing stiffness parallel to the shearing direction. The roughness of fault planes can cause slip in the shear direction to be accompanied by fault-normal movement, working against stiffness in the fault-normal direction. In this dataset, we report on laboratory friction experiments in which we systematically vary the stiffness surrounding the fault in both the shear-parallel and fault-normal directions, to investigate under which conditions slip instabilities can occur. The experiments were performed using synthetic quartz powder in a single-direct shear device. We report the frictional strength, the frictional sliding stability following the rate-and-state frictional framework, and statistics of the slip events. Reducing the shear-parallel stiffness causes the known transition from stable sliding to slow slip to fast stick-slip, whereas reducing the fault-normal stiffness causes stick-slip instabilities without transitional slow events, and reduced stiffness in both directions produces complex behavior.
    Keywords: Center for Marine Environmental Sciences; fault stiffness; friction; laboratory friction experiments; MARUM; slip stability
    Type: Dataset
    Format: application/zip, 3 datasets
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  • 8
    Publication Date: 2024-03-22
    Keywords: Center for Marine Environmental Sciences; Critical slip distance; Critical slip distance, standard deviation; Experiment; fault stiffness; friction; Friction direct effect; Friction direct effect, standard deviation; Friction evolutionary effect, b1; Friction evolutionary effect b1, standard deviation; Initial friction coefficient; Initial friction coefficient, standard deviation; laboratory friction experiments; Linear detrending; Machine stiffness; Machine stiffness, standard deviation; MARUM; Normal stiffness; Normal stiffness/Shear stiffness ratio; Normal Stress; Plot; see reference(s); Shear stiffness; Sliding velocity, final; Sliding velocity, initial; slip stability; Stiffness; Velocity-dependent friction parameter
    Type: Dataset
    Format: text/tab-separated-values, 2442 data points
    Location Call Number Limitation Availability
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  • 9
    Publication Date: 2024-04-20
    Description: Sediment cores were collected with a gravity corer and a multi corer from several sites at the Sartori Mud Volcano in the Calabrian accretionary prism (Mediterranean Sea) during R/V Sonne expedition SO278. Here we present core descriptions of GeoB24302-2 (GC01). To capture the sedimentary structure, gravity cores were longitudinally split directly after recovery on board of cruise SO278 and the archive halves were photographed using the smartCIS1600 line scan technique of the MARUM GeoB Core repository at a 500-dpi resolution. To investigate lithological changes in more detail, macroscopic core descriptions are prepared for all cores. The core descriptions provide information about core length, position, water depth, core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
    Keywords: Center for Marine Environmental Sciences; Core Description; GeoB; GeoB24365-1; GPF 19-2-007H; Lithology; MARUM; Mediterranean Sea; MUC; MultiCorer; R/V SONNE; SO278; SO278_65-1; Sonne_2
    Type: Dataset
    Format: application/pdf, 2.1 MBytes
    Location Call Number Limitation Availability
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  • 10
    Publication Date: 2024-04-20
    Description: Sediment core GeoB24375-1 (GC37) was collected during R/V Sonne expedition SO278 using a gravity corer. The position is close to the Sartori Mud Volcano located in the Calabrian accretionary prism (Mediterranean Sea). To capture the sedimentary structure, the gravity core was longitudinally split directly after recovery on board of cruise SO278 and the archive halve was photographed using the smartCIS1600 line scan technique of the MARUM GeoB Core repository at a 500-dpi resolution. To investigate lithological changes in more detail, a macroscopic core description is prepared. The core description provides information regarding core length, exact position, water depth, number of core sections, core image, color, lithology, sedimentary structures and a descriptive text. Sediment color was determined qualitatively using Munsell soil color charts.
    Keywords: Center for Marine Environmental Sciences; Core Description; GC; GeoB; GeoB24375-1; GPF 19-2-007H; Gravity corer; Lithology; MARUM; Mediterranean Sea; R/V SONNE; Sartori mud volcano; SO278; SO278_75-1; Sonne_2
    Type: Dataset
    Format: application/pdf, 2.3 MBytes
    Location Call Number Limitation Availability
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