GLORIA

GEOMAR Library Ocean Research Information Access

feed icon rss

Ihre E-Mail wurde erfolgreich gesendet. Bitte prüfen Sie Ihren Maileingang.

Leider ist ein Fehler beim E-Mail-Versand aufgetreten. Bitte versuchen Sie es erneut.

Vorgang fortführen?

Exportieren
Filter
Verlag/Herausgeber
Sprache
Erscheinungszeitraum
  • 1
    Online-Ressource
    Online-Ressource
    San Diego :Elsevier,
    Schlagwort(e): Archaeological geology. ; Electronic books.
    Materialart: Online-Ressource
    Seiten: 1 online resource (850 pages)
    Ausgabe: 1st ed.
    ISBN: 9780128156872
    DDC: 551.4637072
    Sprache: Englisch
    Anmerkung: Front Cover -- Geological Records of Tsunamis and Other Extreme Waves -- Geological Records of Tsunamis and Other Extreme Waves -- Copyright -- Contents -- Contributors -- About the Editors -- Preface -- 1 -Introduction -- 1 - Geological records of tsunamis and other extreme waves: concepts, applications and a short history of research -- Introduction -- Disciplinary background -- A short history of paleotsunami research -- Scope of the book -- Outline of the book -- Concluding remarks -- References -- 2 - Historical records: their importance in understanding and mitigating tsunamis -- Introduction -- Catalogues and databases -- Historical records: importance and limitation -- References -- 3 - Tsunami magnitude scales -- Introduction -- Tsunami magnitude scales: an overview -- Relation between tsunami magnitude and intensity -- Possibilities and limitations of tsunami magnitude scales -- Applicability of tsunami magnitude, Mt, to the case of October 25, 2018, earthquake -- Discussion and conclusions -- References -- 4 - Trigger mechanisms and hydrodynamics of tsunamis -- Trigger mechanisms -- Earthquakes -- Landslides -- Volcanism -- Impacts -- Complex trigger -- Hydrodynamics -- Propagation of tsunamis -- Wave deformation in shallow waters (shoaling) -- Inundation and runup -- Backwash -- References -- 5 - Tsunami databases -- Introduction -- Definition -- Database development -- Problems -- Challenges to creating a global tsunami database -- Paleotsunami data -- Structure -- Definition -- Validity -- Other attributes -- Opportunities -- References -- 6 - Onshore archives of tsunami deposits -- Introduction -- Onshore archives of tsunami deposits -- Low-lying coastal plains -- Marshes and estuaries -- Swales within beach-ridge plains -- Lagoons -- Coastal lakes -- Coastal sediment sections -- Beaches (back-beach environments) -- Caves. , Summary -- References -- 2 -Field methods -- 7 - Geophysical prospection and sedimentological characteristics of subaquatic tsunami deposits -- Introduction -- Why do we need research on offshore tsunami deposits? -- Methods to detect offshore tsunami deposits -- Sidescan sonar -- Multibeam echosounder -- Reflection seismic -- LiDAR measurements -- Sampling of offshore tsunami deposits -- Diagnostic criteria of offshore tsunami deposits -- Distribution of offshore tsunami deposits: case studies from different regions -- Conclusions -- References -- 8 - Ground-penetrating radar (GPR) in coastal hazard studies -- Introduction -- The GPR technique -- Theory of GPR and its application in coastal environments -- Data collection and processing -- Recent advancements -- Types of surveys -- Processing -- GPR use in studying past storms and tsunamis -- Erosional records -- Other research areas of methodology development -- Thin-bed studies -- Use of amplitude variation with offset (AVO) -- Multiconfiguration surveys -- Attribute analysis -- 3D modeling of GPR data -- Conclusions -- References -- 9 - Mapping of subaerial coarse clasts -- Introduction -- Aerial and satellite imagery -- Single-point to multi-point measurements -- Photogrammetry and Structure-from-Motion -- Laser scanning -- Point-cloud analysis -- Summary -- References -- 10 - Post-event field surveys -- Introduction and aims -- Overview of how to approach the development, deployment and activity of a post-event field survey -- Before the survey -- During the survey -- After the survey -- Summary reflections on the tasks/issues associated with organizing and undertaking a post-event field survey -- On the evolving "tool kit" of methods available to support post-event field surveys, including those from the broader geolo. , Reflections on the tensions and challenges a post-event field survey team leader might encounter -- Meeting my own and other's expectations -- Time -- Dealing with the unexpected -- Difficult emotions -- Conclusions -- References -- 3 -Fine-grained deposits -- 11 - The sedimentology and geometry of fine-grained tsunami deposits from onshore environments -- Introduction -- Methods -- Fine-grained onshore tsunami deposits -- Depositional features -- Horizontal trends -- Grain-size distribution -- Stratification -- Accumulation of components -- Vertical structures -- Asymmetrical structures that indicate flow direction -- Soft-sediment deformation -- Erosional features -- Discussion -- Conclusions -- References -- 12 - Foraminifera in tsunami deposits -- Characteristics of coastal foraminifera -- Field methods -- Modern foraminifera sampling -- Tsunami and paleotsunami foraminifera sampling -- Laboratory methods -- Sample preparation and foraminiferal analysis -- Foraminifera taxonomy -- Foraminifera test size -- Foraminifera taphonomy -- Statistical techniques -- Example application of foraminifera to tsunami studies -- Current challenges -- Summary of foraminifera use in tsunami research -- References -- 13 - Ostracoda in extreme-wave deposits -- Introduction -- Who are the Ostracoda? -- Taxonomy -- Distribution -- Preservation and taphonomy -- Methods -- Field-based methods -- Baseline ostracod fauna and ecologies -- Deposit sampling -- Lab-based methods -- Post-laboratory methods -- Distinguishing between overwash mechanisms -- Conclusions -- References -- 14 - Diatoms in tsunami deposits -- Introduction: physical and ecological characteristics of diatoms -- Diatoms in tsunami deposits -- Allochthonous diatoms in tsunami deposits, indicators for sediment provenance -- Diatoms as indicators of tsunami runup extent. , Sorting of diatom valves in tsunami deposits -- Preservation of diatom valves in tsunami deposits -- Comparison of diatoms in tsunami and storm-surge deposits -- Recommendations for investigating a candidate tsunami deposit -- Field work and data collection -- Laboratory processing and analyses -- Appendix 1: common diatoms reported in tsunami deposits -- Appendix 2: published criteria for identifying tsunami deposits using diatoms -- Appendix 3: diatom slide preparation and counting -- Appendix 4: assessment of diatom preservation -- References -- 15 - The application of molluscs for investigating tsunami deposits -- Introduction -- The use of molluscs in paleotsunami research -- Characteristics of mollusc species assemblages in tsunami deposits -- Paleo-current flow direction -- Infaunality as a proxy for erosion depth -- Shell size -- Taphonomic processes -- Shell material -- Taphonomic characteristics -- Differences between coastal and offshore settings -- Geochemical analysis -- Differentiating between tsunami and storm deposits -- Conclusions -- References -- 16 - Magnetic susceptibility and anisotropy of magnetic susceptibility: versatile tools to decipher hydrodynamic ch ... -- Introduction -- The principles of the anisotropy of magnetic susceptibility -- Magnetic susceptibility of tsunami deposits -- Anisotropy of magnetic susceptibility -- Methodology -- Sediment sampling in the field -- Caution and limits -- Sediment sampling in the laboratory -- Field experiments -- Laboratory measurements -- Contribution of MS/AMS to deciphering tsunami deposits -- Environmental magnetism of tsunami deposits -- Magnetic signatures of tsunami deposits -- Limitations and perspectives -- Contribution of AMS to reconstruct the hydrodynamic conditions for the 2004 Indian Ocean Tsunami flooding at Banda Aceh, Su ... -- Limitations of the method -- Conclusions. , References -- 17 - X-ray tomography applied to tsunami deposits -- Principles of X-ray tomography -- Application to tsunami deposits -- Sampling strategy -- Image analysis -- X-ray anatomy of tsunami deposits -- Internal structure of the deposit and bedforms -- Soft and fine-grained fraction: soil and mud -- Vertical trends of grain size -- Sedimentary fabric -- Distribution of heavy minerals -- Distribution of marine bioclasts -- Conclusions -- References -- 18 - Applications of geochemical proxies in paleotsunami research -- Introduction -- Methods -- Field sampling -- Analytical methods -- Examples and significance of geochemical proxies -- Onshore deposits -- Marine indicators (shell hash, marine carbonate, also seawater) -- Indicators of source material (proxy for mineral composition) -- Grain-size indicator (Zr/K, Rb and K, Si/(K+Ti)) -- Seawater influence and post-diagenetic formation of pyrite (TC, TS, Fe and S) -- Indicator of source material (terrestrial vs. marine/beach) and geochronological marker -- Stable isotopes and C/N -- Biomarkers/organic compounds -- DNA -- Offshore deposits -- Current challenges and potentialities -- Conclusions -- References -- 19 - Microtextures in tsunami deposits: a useful sediment fingerprinting tool -- Introduction -- Methodology -- Laboratory procedure -- Microtextural semi-quantitative classification -- Shape analysis -- Automated microtextural classification -- Case studies -- Boca do Rio (Portugal) -- Arauco and Mataquito (Chile) -- Conclusions -- References -- 20 - Paleogenetic approaches in tsunami deposit studies -- Background -- Pioneering metabarcoding applications in paleotsunami research -- Protocols for sampling and analysis -- Sediment sampling and storage -- Establishment of databases and significance of reference material -- DNA extraction procedures. , Polymerase chain reaction (PCR) and development of specific PCR primers.
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 2
    Schlagwort(e): Archaeological geology ; Tsunamis Research ; Tsunami ; Sediment ; Sedimentation ; Fazies ; Sedimentologie ; Angewandte Geophysik ; Sturmflut ; Tempestit ; Paläoseismologie ; Paläoseismizität ; Feinstratigraphie ; Biostratigraphie ; Tempestit ; Elektromagnetische Reflexionsmethode ; Fossil ; Geochronologie ; Lidar ; Seebeben ; Tempestit ; Stratigraphie
    Materialart: Buch
    Seiten: xxxi, 816 Seiten , Illustrationen, Diagramme, Karten , 24 cm
    ISBN: 9780128156865
    DDC: 551.4637072
    RVK:
    Sprache: Englisch
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 3
    Schlagwort(e): Geschichte
    In: Geographische Rundschau 〈Braunschweig〉, Braunschweig : Westermann Bildungsmedien Verlag GmbH, 1949, 61(2009), 12, Seite 4-10, 0016-7460
    In: Geographische Rundschau 61.2009,12, 61(2009), 12, Seite 4-10
    In: volume:61
    In: year:2009
    In: number:12
    In: pages:4-10
    Materialart: Artikel
    ISSN: 0016-7460
    Sprache: Deutsch
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 4
    Publikationsdatum: 2022-10-13
    Beschreibung: Abstract Sabkhas are key landforms along the southern coast of the Arabian Gulf and represent modern analogues for depositional and diagenetic processes controlling properties and quality of ancient hydrocarbon‐bearing carbonates. While previous investigations of coastal sabkhas in Qatar have mainly focused on dolomitization processes, presented here is one of the first studies reconstructing facies changes and coastal formation in great detail. In the sabkha of Al‐Kharayej (Gulf of Salwa), fifteen different facies types were distinguished based on twelve sediment cores, two trenches, as well as grain‐size distribution, X‐ray powder diffraction, thin section and microfossil analyses. Age estimates were based on seventy‐eight 14C‐AMS and optically stimulated luminescence data. The sabkha parasequence comprises pre‐transgressive dune sands, a thin, transgressive layer of reworked dune material, a mid‐energy open‐coast to open‐lagoon facies, a low‐energy lagoon facies, saline lake facies (salina: swallow‐tail gypsum and gypsum mush) and the supratidal sabkha characterized by diagenetic overprinting (buckled gypsum crusts and halite crust). Transgressive marine flooding created open‐coast to open‐lagoon sedimentation after ca 7000 cal yr bp, followed by initial spit formation at the northern sabkha end at the beginning of the relative sea‐level highstand (6000 cal yr bp). This main outer spit prograded southward and a more narrow, low‐energy spit, diverted landward, closing a small lagoon in the northern sabkha 4500 to 4000 cal yr bp. The falling relative sea‐level and longshore drift intensified the southward extension and widening of the main spit, and the main lagoon became more shallow. At 2000 to 1500 cal yr bp, the outer spit had almost closed the main lagoon, leading to salina and, finally, sabkha conditions. It is shown how specific local conditions (coastline orientation; wind, wave, tidal energy, longshore drift; depositional relief; sediment sources) created a spit‐controlled sabkha that is genetically distinct from the classical model of shore‐perpendicular accumulation of coarser sediment during high tides or storms.
    Beschreibung: Universität zu Köln
    Beschreibung: ExxonMobil Research Qatar
    Beschreibung: Ruprecht Karls Universitaet Heidelberg
    Schlagwort(e): ddc:552.5
    Sprache: Englisch
    Materialart: doc-type:article
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 5
    Publikationsdatum: 2023-12-02
    Beschreibung: The dataset summarizes measurement data that were used to calculate OSL rock surface exposure ages for wave-emplaced coastal boulders at the Rabat coast (Morocco). It consists of sensitivity-corrected natural luminescence signals (Lx/Tx values) from the surfaces of 17 rock samples. For each sample Lx/Tx values for the uppermost 15 mm are presented in 1-mm steps. Each of these values is the average of 3-5 individual measurements from the same depth level. The chronological information inferred from this dataset can be used to characterise recurrence patterns of storms and tsunamis at the Atlantic coast of Morocco.
    Schlagwort(e): coastal boulder; Depth, relative; Event label; Luminescence, normalized; Luminescence, normalized, error; luminescence rock surface dating; Morocco; Morocco, North Africa; Rabat_coast_HAR_1-1; Rabat_coast_HAR_1-1_CAL; Rabat_coast_HAR_2-1; Rabat_coast_HAR_3-1; Rabat_coast_RAB_1-1; Rabat_coast_RAB_1-2; Rabat_coast_RAB_5-1; Rabat_coast_RAB_5-1_CAL; Rabat_coast_TEM_2-1; Rabat_coast_TEM_3-1; Rabat_coast_TEM_3-1_CAL; Rabat_coast_TEM_4-1; Rabat_coast_VAL_1-1; Rabat_coast_VAL_1-2; Rabat_coast_VAL_4-1; Rabat_coast_VAL_4-1_CAL_1; Rabat_coast_VAL_6-1; Risø TL/OSL DA20 luminescence reader used with: post-IRSL-BSL protocols; ROCK; Rock sample; Sample ID; storm; surface exposure dating; tsunami
    Materialart: Dataset
    Format: text/tab-separated-values, 1016 data points
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 6
    Publikationsdatum: 2024-02-06
    Beschreibung: Lake Ladoga in northwestern Russia is Europe's largest lake. The postglacial history of the Ladoga basin is for the first time documented continuously with high temporal resolution in the upper 13.3 m of a sediment core (Co1309) from the northwestern part of the lake. We applied a multiproxy approach including (bio‐)geochemical and granulometric analyses. The dataset comprises grain-size data (clay, silt, sand), biogeochemical data (total organic carbon (TOC), total sulphur (TS)), water content and XFR data (Fe, P, Ti, K, Zr, Ti/Al, Rb/Sr, Zr/Rb) of the composit profile of sediment core Co1309 as presented in Gromig et al. 2019.
    Schlagwort(e): AWI_Envi; Geochemistry; Lake Ladoga; lake sediments; PLOT-Project; Polar Terrestrial Environmental Systems @ AWI; Sediment core
    Materialart: Dataset
    Format: application/zip, 3 datasets
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 7
    Publikationsdatum: 2024-02-06
    Schlagwort(e): AWI_Envi; Carbon, organic, total; Co1309; Core; CORE; Core section label; DEPTH, sediment/rock; Geochemistry; Ladoga Lake, Russia; Lake Ladoga; lake sediments; PLOT-Project; Polar Terrestrial Environmental Systems @ AWI; Sediment core; Sulfur, total; Water content, volumetric
    Materialart: Dataset
    Format: text/tab-separated-values, 380 data points
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 8
    Publikationsdatum: 2024-02-06
    Schlagwort(e): AWI_Envi; Co1309; Core; CORE; Core section label; DEPTH, sediment/rock; Geochemistry; Iron; Ladoga Lake, Russia; Lake Ladoga; lake sediments; Phosphorus; PLOT-Project; Polar Terrestrial Environmental Systems @ AWI; Potassium; Rubidium/Strontium ratio; Sediment core; Titanium; Titanium/Aluminium ratio; Zirconium; Zirconium/Rubidium ratio
    Materialart: Dataset
    Format: text/tab-separated-values, 59178 data points
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 9
    Publikationsdatum: 2024-02-06
    Schlagwort(e): AWI_Envi; Clay; Co1309; Core; CORE; Core section label; DEPTH, sediment/rock; Geochemistry; Ladoga Lake, Russia; Lake Ladoga; lake sediments; PLOT-Project; Polar Terrestrial Environmental Systems @ AWI; Sand; Sediment core; Silt
    Materialart: Dataset
    Format: text/tab-separated-values, 380 data points
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
  • 10
    Publikationsdatum: 2020-06-14
    Beschreibung: Lake Ladoga hosts preglacial sediments, although the Eurasian ice sheet overrode the area during the LGM . These sediments were first discovered by a seismic survey and are investigated using a 22.75‐m‐long core. Its upper 13.30 m comprise Holocene and Lateglacial sediments separated from the lower 11.45 m of preglacial sediments by a hiatus. They consist of highly terrigenous lacustrine sediments, which according to OSL dating, were deposited during an early stage of the last ice age (MIS 5). The palynological data allow a first reconstruction of the Early Weichselian environmental history for northwestern Russia. Birch and alder forests with broad‐leaved taxa dominated during MIS 5d (c . 118–113 ka), suggesting a climate more favourable than in the Holocene. A high content of well‐sorted sands and poorly preserved palynomorphs indicates a shallow‐water environment at least temporarily. More fine‐grained sediments and better preserved organic remains suggest deeper water environments at the core location during MIS 5c (c . 113–88 ka). Pine and spruce became dominant, while broad‐leaved taxa started to disappear, especially after c . 90 ka, pointing to a gradual climate cooling. An increase in open herb‐dominated habitats at the beginning of MIS 5b (c . 88–86 ka) reflects a colder and dryer climate. However, later (c . 86–82 ka) pine and spruce again became more common. Birch and alder forests dominated in the area c . 82–80 ka (beginning of MIS 5a). Although open treeless habitats also became more common at this time, a slight increase in hazel may point to somewhat warmer climate conditions coinciding with the beginning of MIS 5a. The studied sediments also contain numerous remains of freshwater algae and cysts of marine and brackish‐water dinoflagellates and acritarchs documenting that the present lake basin was part of a brackish‐water basin during the Early Weichselian, probably as a gulf of the Pre‐Baltic Sea.
    Repository-Name: EPIC Alfred Wegener Institut
    Materialart: Article , isiRev
    Standort Signatur Einschränkungen Verfügbarkeit
    BibTip Andere fanden auch interessant ...
Schließen ⊗
Diese Webseite nutzt Cookies und das Analyse-Tool Matomo. Weitere Informationen finden Sie hier...