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  • 1
    Keywords: Forschungsbericht ; Eurasien Nord ; Ladogasee ; Holozän ; Paläoklima
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource (73 Seiten, 89,98 MB) , Illustrationen, Diagramme
    Language: German
    Note: Förderkennzeichen BMBF 03G0859A-C. - Verbund-Nummer 01161585 , Unterschiede zwischen dem gedruckten Dokument und der elektronischen Ressource können nicht ausgeschlossen werden
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  • 2
    In: Marine geology, Amsterdam [u.a.] : Elsevier Science, 1964, 263(2009), 1/4, Seite 97-107, 1872-6151
    In: volume:263
    In: year:2009
    In: number:1/4
    In: pages:97-107
    Description / Table of Contents: Newly acquired bathymetric and seismic reflection data have revealed mass-transport deposits (MTDs) on the northeastern Cretan margin in the active Hellenic subduction zone. These include a stack of two submarine landslides within the Malia Basin with a total volume of approximately 4.6 km3 covering an area of about 135 km2. These two MTDs have different geometry, internal deformations and transport structures. The older and stratigraphic lower MTD is interpreted as a debrite that fills a large part of the Malia Basin, while the second, younger MTD, with an age of at least 12.6 cal. ka B.P., indicate a thick, lens-shaped, partially translational landslide. This MTD comprises multiple slide masses with internal structure varying from highly deformed to nearly undeformed. The reconstructed source area of the older MTD is located in the westernmost Malia Basin. The source area of the younger MTD is identified in multiple headwalls at the slopebasin-transition in 450 m water depth. Numerous faults with an orientation almost parallel to the southwestnortheast-trending basin axis occur along the northern and southern boundaries of the Malia Basin and have caused a partial steepening of the slopebasin-transition. The possible triggers for slope failure and mass-wasting include (i) seismicity and (ii) movement of the uplifting island of Crete from neotectonics of the Hellenic subduction zone, and (iii) slip of clay-mineral-rich or ash-bearing layers during fluid involvement.
    Type of Medium: Online Resource
    Pages: graph. Darst
    ISSN: 1872-6151
    Language: English
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  • 3
    In: Quaternary science reviews, Amsterdam [u.a.] : Elsevier, 1982, 28(2009), 15/16, Seite 1555-1567, 0277-3791
    In: volume:28
    In: year:2009
    In: number:15/16
    In: pages:1555-1567
    Description / Table of Contents: Lake Van is the fourth largest terminal lake in the world (volume 607 km3, area 3570 km2, maximum depth 460 m), extending for 130 km WSWENE on the Eastern Anatolian High Plateau, Turkey. The sedimentary record of Lake Van, partly laminated, has the potential to obtain a long and continuous continental sequence that covers several glacialinterglacial cycles (ca 500 kyr). Therefore, Lake Van is a key site within the International Continental Scientific Drilling Program (ICDP) for the investigation of the Quaternary climate evolution in the Near East (‘PALEOVAN’). As preparation for an ICDP drilling campaign, a site survey was carried out during the past years. We collected 50 seismic profiles with a total length of ~850 km to identify continuous undisturbed sedimentary sequences for potential ICDP locations. Based on the seismic results, we cored 10 different locations to water depths of up to 420 m. Multidisciplinary scientific work at positions of a proposed ICDP drill site included measurements of magnetic susceptibility, physical properties, stable isotopes, XRF scans, and pollen and spores. This core extends back to the Last Glacial Maximum (LGM), a more extended record than all the other Lake Van cores obtained to date. Both coring and seismic data do not show any indication that the deepest part of the lake (Tatvan Basin, Ahlat Ridge) was dry or almost dry during past times. These results show potential for obtaining a continuous undisturbed, long continental palaeoclimate record. In addition, this paper discusses the potential of "PALEOVAN" to establish new results on the dynamics of lake level fluctuations, noble gas concentration in pore water of the lake sediment, history of volcanism and volcanic activities based on tephrostratigraphy, and paleoseismic and earthquake activities.
    Type of Medium: Online Resource
    Pages: Ill., graph. Darst
    ISSN: 0277-3791
    Language: English
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  • 4
    In: Marine geology, Amsterdam [u.a.] : Elsevier Science, 1964, 259(2009), 1/4, Seite 47-58, 1872-6151
    In: volume:259
    In: year:2009
    In: number:1/4
    In: pages:47-58
    Description / Table of Contents: Continental shelves represent areas of highest economical and ecological importance. Nevertheless, these sedimentary systems remain poorly understood due to a complex interplay of various factors and processes which results in highly individual construction schemes. Previous studies of sedimentary shelf systems have mainly focused on a limited number of cores, retrieved from Holocene fine-grained depocentres. As such, the relation between shelf architecture and sedimentary history remains largely obscure. Here, we present new data from the NW Iberian shelf comprising shallow-seismic profiles, a large number of sediment cores, and an extended set of radiocarbon dates to reveal the Late Quaternary evolution of a low-accumulation shelf system in detail. On the NW Iberian shelf, three main seismic units are identified. These overly a prominent erosional unconformity on top of the basement. The lowermost Unit 1 is composed of maximal 75-m thick, Late Tertiary to Pleistocene deposits. The youngest sediments of this unit are related to the last glacial sea-level fall. Unit 2 was controlled by the deglacial sea-level rise and shows a maximum thickness of 15 m. Finally, Unit 3 comprises deposits related to the late stage of sea-level rise and the modern sea-level highstand with a thickness of 4 m in mid-shelf position. Two pronounced seismic reflectors separate these main units from each other. Their origin is related to (1) exposure and ravinement processes during lower sea level, and (2) to reworking and re-deposition of coarse sediments during subsequent sea-level rise. According to the sediment core ground-truthing, sediments of the Late Tertiary to Pleistocene unit predominantly display homogenous fine sands with exceptional occurrences of palaeosols that indicate an ancient exposure surface. Fine sands which were deposited in the run of the last sea-level rise show a time-transgressive retrogradational development. The seismic reflectors, bounding the individual units, appear in the cores as 0.1 to 1-m thick deposits consisting either of shell gravels or siliceous coarse sands with gravels. The modern sea-level highstand stage is characterised by zonal deposition of mud forming a mud belt in mid-shelf position, and sediment starvation on outer shelf zones. Radiocarbon ages indicate that this mud belt was the main depocentre for river-supplied fine material on the NW Iberian shelf at least over the past 5.32 ka BP. The initial onset of this depocentre is proposed to be related to a shift in the balance between rate of sea-level rise and amount of terrigenous sediment supply. Various other stratigraphical shelf reconstructions reveal analogies in architecture which indicate that timing and shaping of the individual units on low-accumulation shelves is fundamentally controlled by eustatic sea-level changes. Other factors of local importance such as differential elevation of the basement and the presence of morphological barriers formed by rocky outcrops on the seafloor have additionally modifying influence on the sedimentary processes.
    Type of Medium: Online Resource
    Pages: Ill., graph. Darst
    ISSN: 1872-6151
    Language: English
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  • 5
    Online Resource
    Online Resource
    Kiel : Ozean der Zukunft, Die Kieler Meereswissenschaften
    Keywords: Hochschulschrift
    Type of Medium: Online Resource
    Pages: Online-Ressource ( PDF-Datei : 24 S., 1,3 MB) , Ill.
    Series Statement: Kinder- und Schüleruni Kiel : für Schülerinnen und Schüler von 8 bis 16 Jahren 2009.06,30
    Language: German
    Note: Auch als gedr. Dokument vorh
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  • 6
    Keywords: Hochschulschrift ; Chile Süd ; Neotektonik ; Strukturgeologie
    Type of Medium: Online Resource
    Pages: Online-Ressource (PDF-Datei: V, 73 S., 25,8 MB) , graph. Darst.
    Language: English , German
    Note: Enth. Zeitschriften-Aufsätze , Kiel, Univ., Diss., 2011
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  • 7
    Keywords: Hochschulschrift ; Ohridsee ; Sedimentation ; Neotektonik ; Hydroakustik ; Seismik
    Type of Medium: Online Resource
    Pages: Online-Ressource (Online-Ressource)
    DDC: 550
    Language: English
    Note: Kiel, Univ., Diss., 2012
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  • 8
    In: Marine geology, Amsterdam [u.a.] : Elsevier Science, 1964, 271(2010), 1/2, Seite 44-54, 1872-6151
    In: volume:271
    In: year:2010
    In: number:1/2
    In: pages:44-54
    Description / Table of Contents: In this study we aim on a reconstruction of mechanisms and kinematics of slope-failure and mass-movement processes along the northeastern slope of Crete in the Hellenic forearc, eastern Mediterranean. Here, subsidence of the forearc basin and the uplift of the island of Crete cause ongoing steepening of the slope in-between. The high level of neotectonic activity in this region is expected to exert a key role in slope-failure development. Newly acquired reflection seismic data from the upper slope region reveal an intact sediment cover while the lower slope is devoid of both intact strata and mass-transport deposits (MTDs). In a mid-slope position, however, we found evidence for a not, vert, similar 4-km3-sized landslide complex that comprises several MTDs from translational transport of coherent sediment bodies over short distances. Morphometric analysis of these MTDs and their source scars indicates that this part of the northeast Cretan slope can be characterized as a cohesive slope. Furthermore, we reconstruct retrogressive development for this complex and determine a critical slope angle for both pre-conditioning of failure and subsequent landslide deposition near source scars. Consequently, data imply that the investigated shallower slope is stable due to low angles in the order of 3°, whereas 5°-inclined mid-slope portions favour both slope destabilization and landslide deposition. The failed mid-slope parts are dominated by sediment truncations from faults almost correlating with the orientation of head- and sidewalls of scars. We suggest that cohesive landslides and MTDs are generated and preserved, respectively, in such critical slope regions. If once generated, cohesive landslides reach the lower slope further downslope that exceeds the threshold gradient for MTD deposition (not, vert, similar 5°), they are transported all the way down to the foot of the slope and disintegrate to mass flows. From these observations we suggest that the mass-wasting history of the investigated Cretan slope area over a longer period of time is characterized by repeated sediment erosion and transport into the deeper Cretan Sea basin. The relocation of the critical slope portion in upslope direction and therefore recurrence of mass-wasting events is thereby likely controlled by the progressive steepening of the slope. This mechanism and restriction of sediment failure to narrow, critically-inclined and relocating slope portions likely explains how such an active margin setting can exhibit only scarce findings of MTDs on the slope despite an expected, extensive and widespread mass wasting.
    Type of Medium: Online Resource
    Pages: graph. Darst
    ISSN: 1872-6151
    Language: English
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  • 9
    In: Quaternary research, Cambridge : Cambridge University Press, 1970, 73(2010), 2, Seite 385-392, 1096-0287
    In: volume:73
    In: year:2010
    In: number:2
    In: pages:385-392
    Description / Table of Contents: The relationship of sea-level changes and short-term climatic changes with turbidite deposition is poorly documented, although the mechanisms of gravity-driven sediment transport in submarine canyons during sea-level changes have been reported from many regions. This study focuses on the activity of the Dakar Canyon off southern Senegal in response to major glacial/interglacial sea-level shifts and variability in the NW-African continental climate. The sedimentary record from the canyon allows us to determine the timing of turbidite events and, on the basis of XRF-scanning element data, we have identified the climate signal at a sub-millennial time scale from the surrounding hemipelagic sediments. Over the late Quaternary the highest frequency in turbidite activity in the Dakar Canyon is confined to major climatic terminations when remobilisation of sediments from the shelf was triggered by the eustatic sea-level rise. However, episodic turbidite events coincide with the timing of Heinrich events in the North Atlantic. During these times continental climate has changed rapidly, with evidence for higher dust supply over NW Africa which has fed turbidity currents. Increased aridity and enhanced wind strength in the southern SaharanSahelian zone may have provided a source for this dust.
    Type of Medium: Online Resource
    Pages: graph. Darst
    ISSN: 1096-0287
    Language: English
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  • 10
    Keywords: Hochschulschrift
    Type of Medium: Book
    Pages: [24] S. , Ill.
    Series Statement: Kinder- und Schüleruni Kiel : für Schülerinnen und Schüler von 8 bis 16 Jahren 2009.06,30
    Language: German
    Note: Auch als elektronisches Dokument vorh
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