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  • PANGAEA  (19)
  • Heidelberg, Germany : Springer-Verlag Berlin Heidelberg  (1)
Document type
Keywords
Language
  • 1
    Online Resource
    Online Resource
    Heidelberg, Germany : Springer-Verlag Berlin Heidelberg
    Keywords: Oceanography ; Physical geography ; Ecology ; Geology ; Oceanography. ; Geology. ; Ecology . ; Physical geography. ; Geophysics. ; Oceanography ; Wörterbuch ; Meeresgeologie ; Meereskunde ; Meeressediment ; Mineralischer Rohstoff ; Wörterbuch ; Meeressediment ; Turbidit ; Dichteströmung ; Fazies ; Sedimentologie ; Sedimentation ; Meeresboden ; Cold Seep ; Methan ; Schlammvulkan ; Submariner Vulkanismus ; VHMS-Lagerstätte ; Schwarzer Raucher ; Weisser Raucher
    Description / Table of Contents: Abyssal plain -- Accretionary wedge -- Acidification -- Active continental margin -- Anoxic oceans -- Asphalt volcanism -- Axial magma chamber -- Axial summit graben, axial summit trough -- Backarc basins and backarc spreading center -- Beach -- Beach nourishment -- Beach processes -- Biochronology -- Biogenic barium -- Biostratigraphy -- Bioturbation -- Black and white smoker -- Boninites -- Bottom simulating seismic reflector (BSR) -- Bottom-boundary layer -- Bouma sequence -- Break waters -- Carbon dioxide and climate (carbon cycle) -- Carbon isotopes/-stratigraphy -- Carbon pump -- Carbonate dissolution -- Carbonate factory -- CCD -- Chemosynthetic life -- Clay minerals -- Coastal bio-geochemical cycles -- Coastal engineering -- Coasts -- Cold seeps -- Continental margin sediments -- Continental rift system, graben -- Continental rise -- Continental slope -- Contour currents -- Convergence texture of seismic reflectors -- Core-complex formation -- Crustal accretion (incl. gabbro glacier model) -- Cumulate -- Curie temperature -- Currents -- Data banks (Pangaea) -- Decollement -- Deep biosphere -- Deep Sea Fans -- Deep sea sediments -- Delta -- Depleted mantle -- Detachment fault -- Diatoms -- Dinoflagellates -- Driving forces (slab pull, ridge push) -- Dunes -- Dust in the ocean -- Dykes -- Earthquake -- El Nino -- Energy resources -- Epicenter, hypocenter -- Erosion and hiatusses -- Estuary, estuarine/anti-estuarine current system -- Eustasy -- Events in ocean history -- Explosive volcanism in the deep sea -- Export production -- Fault-plane solution -- Fjord -- Foraminifers (benthic) -- Foraminifers (planktonic) -- Forebulge (lithospheric) -- Fracture zone -- Fresh water in the oceans -- Gabbro -- Gas hydrates -- GEBCO -- Geochronology -- Geohazards (coastal disasters) -- Geological effects of ocean circulation -- Geomagnetic field -- Glacial marine sedimentation -- Glacio-isostatic adjustment -- Gravity field -- Grounding line -- Groynes -- Guyot, atoll -- Heat flow -- High-pressure/low temperature metamorphism -- History of Marine Geology -- Hot spots and mantle plumes -- Hurricanes/ Typhoons -- Hydrocarbons (natural oil and gas) -- Hydrothermalism -- Hydrothermal plumes -- Hydrothermal vent fluids -- IBCAO -- Ice rafted debris (IRD) -- Impacts and their products -- Integrated Coastal Zone Management -- Intracontinental rifting -- Intraoceanic subduction zone -- Intraplate volcanism -- Island arc volcanism, volcanic arcs -- Lagoon -- Laminated sediments -- Large igneous provinces (LIP) -- Lava types (pillow lava, sheet flows, lobate, etc) -- Layering of oceanic crust -- Lithosphere -- Lithospheric mantle -- Lithostratigraphy -- Magmatism at convergent plate boundaries -- Magnetostratigraphy -- Magnetism and paleomagnetism -- Manganese crusts, Co-rich manganese crusts -- Manganese nodules -- Mangrove coast -- Mantle plume -- Marginal seas -- Marine evaporites -- Marine microfossils -- Marine mineral resources -- Marine sedimentary basins -- Mass wasting (slides) -- Methane in sediments -- Mid-ocean ridges -- Mid-ocean ridge magmatism -- Milankovitch frequencies/-cyclicities -- Modelling past oceans -- Modern analog technique -- Mohorovicic-discontinuity (Moho) -- Morain -- Morphology of a subuction zone (forearc, backarc, deep sea trench) -- Mud volcano -- Nannoplankton/ coccolithophorids -- Nitrogene (stable) isotopes -- North Atlantic Oscillation (NAO) -- Oceanic crust -- Ocean drilling -- Ocean margin systems -- Oceanic rift system, Mid-Oceanic Ridge -- Oil spill -- Ophiolite -- Organic matter -- Orogeny -- Overlapping spreading center -- Oxygen isotopes and –stratigraphy -- Paired metamorphic belt -- Paleoceanographic proxies -- Paleoceanography -- Paleophysiography of ocean basins -- Paleoproductivity -- Passive plate margin -- Peridotite -- Petroleum, natural gas -- phosphorites -- Placer deposits -- Plate motion -- Plate stratigraphy -- Pollen/spores -- Precambrian ocean basins -- Propagating rift -- Pteropods -- Pull-apart basin -- Push-up block -- Radiocarbon dating -- Radiogenic tracers -- Radiolarians -- Reef coast -- Reefs -- Regional marine geology -- Regional oceanography and sediments -- Reflection/refraction seismology -- Regression -- Relative sea level (RSL) cycle -- Ridge-plume interaction -- Salt domes in the ocean -- Sapropel -- Sclerochronology -- Sea floor spreading -- Sea level dynamics -- Sea walls / revetments -- Seamounts -- Sediment dynamic -- Sediment transport models -- Sedimentary Sequence / parasequence -- Seismic layers -- Seismogenic zone -- Sequence stratigraphy -- Serpentinization -- Shelf -- Silica -- Source rocks, reservoirs -- Spreading axis -- Spreading rates and ridge morphology -- Stratigraphy (table) -- Subduction -- Subduction erosion -- Submarine canyon -- Subsidence -- Systems tracts (highstand, lowstand, transgressive, shelf margin) -- Technology in marine geosciences -- Terrane -- Tidal coast -- Transform fault -- Transgression -- Triple junction -- Tsunamis -- Turbidite / contourite -- Underwater archaeology -- Upwelling in the ocean and its geological effects -- Volcanic eruptions as hazards -- Volcanism and climate -- Volcanogenic massive sulfides -- Wadati- Benioff-zone -- Wadden Sea -- Waves -- Wilson cycle
    Type of Medium: Online Resource
    Pages: 1 Online-Ressource
    ISBN: 9789400766440
    Series Statement: Earth Sciences Series
    Language: English
    Location Call Number Limitation Availability
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  • 2
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    Unknown
    PANGAEA
    In:  Supplement to: Lampe, Reinhard; Endtmann, Elisabeth; Janke, Wolfgang; Meyer, Hinrich; Lübke, Harald; Harff, Jan; Lemke, Wolfram (2005): A new relative sea-level curve for the Wismar Bay, N-German Baltic coast. Meyniana, 57, 5-35, https://doi.org/10.2312/meyniana.2005.57.5
    Publication Date: 2023-01-13
    Description: The Baltic coast of Mecklenburg-Vorpommern is located in the transition Zone between the region of Fennoscandian Uplift and the Central European Depression. In relation to the eustatic sea-level rise, the northeast coast shows a slower inundation, while for the southwestern area a faster transgression is indicated, which can be attributed to crustal movements. To determine the spatial and temporal differences since the onset of the Littorina Transgression, three relative sea-level curves have been established along a transect parallel to the gradient of upliftlsubsidence. The Wismar Bay area is one endpoint of the transect demonstrating today 10 Abb., 2 Tab. a relative sea-level rise of 1.4 mm/a. To determine the relative sea-level curve for the Wismar Bay, two sites were investigated on Rustwerder Spit (Poel) and Redentin. They provided reliable depth-age data, while the stratigraphy was additionally supported by lithological/geochemical, pollen, diatom and macrofossil data. Additional evidence was provided by archaeological submarine surveys and excavations. Comparing the new relative sea-level curve with a curve from the Vorpommern coast, it can be shown that for the period from 4000 cal BC until present, the differences between the two curves are caused by a constant neotectonic movement, while for the older periods an increasing isostatic component must be taken into account.
    Keywords: Age; Age, 14C AMS; Age, comment; Age, dated; Age, dated standard deviation; Age, error; Comment; Facies name/code; Sample code/label; Site; wismarbay; Wismar Bay, Baltic Sea, Germany; δ13C
    Type: Dataset
    Format: text/tab-separated-values, 1012 data points
    Location Call Number Limitation Availability
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  • 3
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    Unknown
    PANGAEA
    In:  Supplement to: Perner, Kerstin; Moros, Matthias; Lloyd, Jerry M; Kuijpers, Antoon; Telford, Richard J; Harff, Jan (2011): Centennial scale benthic foraminiferal record of late Holocene oceanographic variability in Disko Bugt, West Greenland. Quaternary Science Reviews, 30(19-20), 2815-2826, https://doi.org/10.1016/j.quascirev.2011.06.018
    Publication Date: 2024-02-02
    Description: A new centennial scale benthic foraminiferal record of late Holocene climate variability and oceanographic changes off West Greenland (Disko Bugt) highlights substantial subsurface water mass changes (e.g. temperature and salinity) of the West Greenland Current (WGC) over the past 3.6 ka BP. Benthic foraminifera reveal a long-term late Holocene cooling trend, which may be attributed to increased advection of cold, low-salinity water masses derived from the East Greenland Current (EGC). Cooling becomes most pronounced from c. 1.7 ka BP onwards. At this point the calcareous Atlantic benthic foraminiferal fauna decrease significantly and is replaced by an agglutinated Arctic fauna. Superimposed on this cooling trend, centennial scale variability in the WGC reveals a marked cold phase at c. 2.5 ka BP, which may correspond to the 2.7 ka BP cooling-event recorded in marine and terrestrial archives elsewhere in the North Atlantic region. A warm phase recognized at c. 1.8 ka BP is likely to correspond to the 'Roman Warm Period' and represents the warmest bottom water conditions. During the time period of the 'Medieval Climate Anomaly' we observe only a slight warming of the WGC. A progressively more dominant cold water contribution from the EGC on the WGC is documented by the prominent rise in abundance of agglutinated Arctic water species from 0.9 ka BP onwards. This cooling event culminates at c. 0.3 ka BP and represents the coldest episode of the 'Little Ice Age'. Gradually increased influence of cold, low-salinity water masses derived from the EGC may be linked to enhanced advection of Polar and Arctic water by the EGC. These changes are possibly associated with a reported shift in the large-scale North Atlantic Oscillation atmospheric circulation pattern towards a more frequent negative North Atlantic Oscillation mode during the late Holocene.
    Keywords: Age; AGE; Baffin Bay; Benthic foraminifera; Dendrochronological crossdating; East Greenland Current; Event label; GC; Gravity corer; GREENClim; Irminger; Islandiella norcrossi; Late Holocene; Maria S. Merian; MSM05/3; MSM05/3_343310-2-2; MSM05/3_343310-5-1; MUC; MultiCorer; NAO; Nonionellina labradorica; Percentage; Ratio; West Greenland Current
    Type: Dataset
    Format: text/tab-separated-values, 1938 data points
    Location Call Number Limitation Availability
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  • 4
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    Unknown
    PANGAEA
    In:  Alfred Wegener Institute, Helmholtz Centre for Polar and Marine Research, Bremerhaven
    Publication Date: 2024-01-12
    Keywords: Calculated; Course; CT; DATE/TIME; HE244; HE244-track; Heincke; LATITUDE; LONGITUDE; Speed; Underway cruise track measurements
    Type: Dataset
    Format: text/tab-separated-values, 3334 data points
    Location Call Number Limitation Availability
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  • 5
    Publication Date: 2024-06-26
    Description: Die Datenpublikation besteht aus den Korngrößenverteilungen von Oberflächensedimenten aus der südlichen Ostsee und umfaßt 7 Korngrößendatensätze gegliedert nach unterschiedlichen Klassen entsprechend der Methoden von Kolb und Koehn mit insgesamt 111025 Korngrößenwerten. Seit Beginn der fünfziger Jahre werden in Warnemünde systematisch Untersuchungen der Sedimente der westlichen Ostsee durchgeführt. Dabei werden die im Institut für Meereskunde der damaligen Akademie der Wissenschaften der DDR und davor im Seehydrographischen Dienst begonnenen Arbeiten am Institut für Ostseeforschung seit seiner Gründung 1992 fortgeführt. Aus Geheimhaltungsgründen standen die Daten vor 1989 für die wissenschaftliche Interpretation nur eingeschränkt zur Verfügung. Um auch diese 'Altdaten' der freien Forschung zugänglich zu machen, wurde 1994-1996 vom BMFT ein Forschungsprojekt gefördert (03F0079A), das die Erschließung und Publikation dieser teilweise kodierten Daten für die Ostseeforschung zum Ziel hatte. Im Laufe des Projektes wurde ein Bearbeitungsschema für die Daten entwickelt, welches generell für das Management von geomarinen Daten am IOW genutzt werden soll.
    Keywords: Baltic Sea; Bottom grab (Peterson); BP; different cruises; DIVER; IOW10; IOW100; IOW1000; IOW10000; IOW100000; IOW100010; IOW100020; IOW100030; IOW100040; IOW100050; IOW100060; IOW100070; IOW100080; IOW100090; IOW10010; IOW100100; IOW100110; IOW100120; IOW100130; IOW100150; IOW100160; IOW100170; IOW100180; IOW100190; IOW10020; IOW100200; IOW100210; IOW100220; IOW100230; IOW100240; IOW100250; IOW100260; IOW100270; IOW100280; IOW100290; IOW10030; IOW100300; IOW100310; IOW100320; IOW100330; IOW100340; IOW100350; IOW100360; IOW100370; IOW100380; IOW100390; IOW10040; IOW100400; IOW100410; IOW100420; IOW100430; IOW100440; IOW100450; IOW100460; IOW100470; IOW100480; IOW100490; IOW10050; IOW100500; IOW100510; IOW100520; IOW100530; IOW100540; IOW100550; IOW100560; IOW100570; IOW100580; IOW100590; IOW10060; IOW100600; IOW100610; IOW100620; IOW100630; IOW100640; IOW100650; IOW100660; IOW100670; IOW100680; IOW100690; IOW10070; IOW100700; IOW100710; IOW100720; IOW100730; IOW100740; IOW100750; IOW100760; IOW100770; IOW100780; IOW100790; IOW10080; IOW100800; IOW100810; IOW100820; IOW100830; IOW100840; IOW100850; IOW100860; IOW100870; IOW100880; IOW100890; IOW10090; IOW100900; IOW100910; IOW100920; IOW100930; IOW100940; IOW100950; IOW100960; IOW100970; IOW100980; IOW100990; IOW1010; IOW10100; IOW101000; IOW101010; IOW101020; IOW101030; IOW101040; IOW101050; IOW101060; IOW101070; IOW101080; IOW101090; IOW10110; IOW101100; IOW101110; IOW101120; IOW101130; IOW101140; IOW101150; IOW101160; IOW101170; IOW101180; IOW10120; IOW101210; IOW101220; IOW101230; IOW101240; IOW101250; IOW101260; IOW101270; IOW10130; IOW10140; IOW10150; IOW101570; IOW101580; IOW10160; IOW10170; IOW10180; IOW10190; IOW1020; IOW10200; IOW10210; IOW10220; IOW10230; IOW102980; IOW102990; IOW1030; IOW10300; IOW103000; IOW103010; IOW103020; IOW103030; IOW103040; IOW103050; IOW103060; IOW103070; IOW103080; IOW103090; IOW10310; IOW103100; IOW103110; IOW103120; IOW103130; IOW103140; IOW103150; IOW103160; IOW103170; IOW103180; IOW103190; IOW10320; IOW103200; IOW103210; IOW103220; IOW103230; IOW103240; IOW103250; IOW103260; IOW103270; IOW103280; IOW103290; IOW10330; IOW103300; IOW103310; IOW103320; IOW103330; IOW103340; IOW103350; IOW103360; IOW103370; IOW103380; IOW103390; IOW10340; IOW103400; IOW103410; IOW103420; IOW103430; IOW103440; IOW103450; IOW103460; IOW103470; IOW103480; IOW103490; IOW10350; IOW103500; IOW103510; IOW103520; IOW103530; IOW103540; IOW103550; IOW103560; IOW103570; IOW103580; IOW103590; IOW10360; IOW103600; IOW103610; IOW103620; IOW103630; IOW103640; IOW103650; IOW103660; IOW103670; IOW103680; IOW103690; IOW10370; IOW103700; IOW103710; IOW103720; IOW103730; IOW103740; IOW103750; IOW103760; IOW103770; IOW103780; IOW103790; IOW10380; IOW103800; IOW103810; IOW103820; IOW103830; IOW103840; IOW103850; IOW103860; IOW103870; IOW103880; IOW103890; IOW10390; IOW103900; IOW103910; IOW103920; IOW103930; IOW103940; IOW103950; IOW103960; IOW103970; IOW103980; IOW103990; IOW1040; IOW10400; IOW104000; IOW104010; IOW104020; IOW104030; IOW104040; IOW104050; IOW104060; IOW104070; IOW104080; IOW104090; IOW10410; IOW104100; IOW104110; IOW104120; IOW104130; IOW104140; IOW104150; IOW104160; IOW104170; IOW104180; IOW104190; IOW10420; IOW104200; IOW104210; IOW104220; IOW104230; IOW104240; IOW104250; IOW104260; IOW104270; IOW104280; IOW104290; IOW10430; IOW104300; IOW104310; IOW104320; IOW104330; IOW104340; IOW104350; IOW104360; IOW104370; IOW104380; IOW104390; IOW10440; IOW104400; IOW104410; IOW104420; IOW104430; IOW104440; IOW104450; IOW104460; IOW104470; IOW104480; IOW104490; IOW10450; IOW104500; IOW104510; IOW104520; IOW104530; IOW104540; IOW104550; IOW104560; IOW104570; IOW104580; IOW104590; IOW10460; IOW104600; IOW104610; IOW104620; IOW104630; IOW104640; IOW104650; IOW104660; IOW104670; IOW104680; IOW104690; IOW10470; IOW104700; IOW104710; IOW104720; IOW104730; IOW104740; IOW104750; IOW104760; IOW104770; IOW104780; IOW104790; IOW10480; IOW104800; IOW104810; IOW104820; IOW104830; IOW104840; IOW104850; IOW104860; IOW104870; IOW104880; IOW104890; IOW10490; IOW104900; IOW104910; IOW104920; IOW104930; IOW104940; IOW104950; IOW104960; IOW104970; IOW104980; IOW104990; IOW1050; IOW10500; IOW105000; IOW105010; IOW105020; IOW105030; IOW105040; IOW105050; IOW105060; IOW105070; IOW105080; IOW105090; IOW10510; IOW105100; IOW105110; IOW105120; IOW105130; IOW105140; IOW105150; IOW105160; IOW105170; IOW105180; IOW105190; IOW10520; IOW105200; IOW105210; IOW105220; IOW105230; IOW105240; IOW105250; IOW105260; IOW105270; IOW105280; IOW105290; IOW10530; IOW105300; IOW105310; IOW105320; IOW105340; IOW105350; IOW105360; IOW105370; IOW105380; IOW105390; IOW10540; IOW105400; IOW105410; IOW105420; IOW105430; IOW105440; IOW105450; IOW105460; IOW105470; IOW105480; IOW105490; IOW10550; IOW105500; IOW105510; IOW105520; IOW105530; IOW105540; IOW105550; IOW105560; IOW105570; IOW105580; IOW105590; IOW10560; IOW105600; IOW105610; IOW105620; IOW105630; IOW105640; IOW105650; IOW105660; IOW105670; IOW105680; IOW105690; IOW10570; IOW105700; IOW105710; IOW105720; IOW105730; IOW105740; IOW105750; IOW105760; IOW105770; IOW105780; IOW10580; IOW105800; IOW105810; IOW105820; IOW105830; IOW105840; IOW105850; IOW105860; IOW105870; IOW105880; IOW105890; IOW10590; IOW105900; IOW105910; IOW105920; IOW105930; IOW105940; IOW105950; IOW105960; IOW105970; IOW105980; IOW105990; IOW1060; IOW10600; IOW106000; IOW106010; IOW106020; IOW106030; IOW106040; IOW106050; IOW106060; IOW106070; IOW106080; IOW106090; IOW10610; IOW106100; IOW106110; IOW106120; IOW106130; IOW106140; IOW106150; IOW106160; IOW106170; IOW106180; IOW106190; IOW10620; IOW106200; IOW106210; IOW106220; IOW106230; IOW106240; IOW106250; IOW106260; IOW106270; IOW106280; IOW106290; IOW10630; IOW106300; IOW106310; IOW106320; IOW106330; IOW106340; IOW106350; IOW106360; IOW106370; IOW106380; IOW106390; IOW10640; IOW106400; IOW106410; IOW106420; IOW106430; IOW106440; IOW106450; IOW106460; IOW106470; IOW106480; IOW106490; IOW10650; IOW106500; IOW106540; IOW106550; IOW106560; IOW106570; IOW106580; IOW106590; IOW10660; IOW106600; IOW106610; IOW106620; IOW106640; IOW106650; IOW106660; IOW106670; IOW106680; IOW106690; IOW10670; IOW106700; IOW106710; IOW106720; IOW106730; IOW106740; IOW106750; IOW106760; IOW106770; IOW106780; IOW106790; IOW10680; IOW106800; IOW106810; IOW106820; IOW106830; IOW106840; IOW106850; IOW106860; IOW106870; IOW106880; IOW106890; IOW10690; IOW106900; IOW106910; IOW106920; IOW106930; IOW106940; IOW106950; IOW106960; IOW106970; IOW106980; IOW106990; IOW1070; IOW10700; IOW107000; IOW107010; IOW107020; IOW107030; IOW107040; IOW107050; IOW107060; IOW107070; IOW107080; IOW107090; IOW10710; IOW107100; IOW107110; IOW107120; IOW107130; IOW107140; IOW107150; IOW107160; IOW107170; IOW107180; IOW107190; IOW10720; IOW107200; IOW107210; IOW107220; IOW107230; IOW107240; IOW107250; IOW107260; IOW107270; IOW107280; IOW107290; IOW10730; IOW107300; IOW107310; IOW107320; IOW107330; IOW107340; IOW107350; IOW107360; IOW107370; IOW107380; IOW107390; IOW10740; IOW107400; IOW107410; IOW107420; IOW107440; IOW10750; IOW107530; IOW107540; IOW107550; IOW107560; IOW107570; IOW107580; IOW107590; IOW10760; IOW107600; IOW107610; IOW107620; IOW107630; IOW107640; IOW107650; IOW107660; IOW107670; IOW107680; IOW107690; IOW10770; IOW107700; IOW107710; IOW107720; IOW107730; IOW107740; IOW107750; IOW107760; IOW107770; IOW107780; IOW107790; IOW10780; IOW107810; IOW107830; IOW107850; IOW107870; IOW107880; IOW107890; IOW10790; IOW107900; IOW107910; IOW107920; IOW107930; IOW107940; IOW107950; IOW107960; IOW107970; IOW107980; IOW107990; IOW1080; IOW10800; IOW108000; IOW108010; IOW108020; IOW108030; IOW108040; IOW10810; IOW108150; IOW108160; IOW108170; IOW108180; IOW108190; IOW10820; IOW108200; IOW108210; IOW108220; IOW108230; IOW108240; IOW108250; IOW108260; IOW108270; IOW108280; IOW108290; IOW10830; IOW108300; IOW108310; IOW108320; IOW108330; IOW108340; IOW108350; IOW108370; IOW108390; IOW10840; IOW108410; IOW108430;
    Type: Dataset
    Format: application/zip, 7 datasets
    Location Call Number Limitation Availability
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  • 6
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    PANGAEA
    In:  Leibniz Institute for Baltic Sea Research, Warnemünde
    Publication Date: 2024-06-26
    Keywords: Baltic Sea System Study; BASYS; Bornholm Basin, Baltic Sea; DEPTH, sediment/rock; Gravity corer (Kiel type); Greyscale value; IOW211630-8; KOT99/97/02.1; Multi-Sensor Core Logger/colorscan/scion image; Petr Kottsov; SL
    Type: Dataset
    Format: text/tab-separated-values, 105252 data points
    Location Call Number Limitation Availability
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  • 7
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    PANGAEA
    In:  Leibniz Institute for Baltic Sea Research, Warnemünde
    Publication Date: 2024-06-26
    Keywords: Baltic Sea System Study; BASYS; Bornholm Basin, Baltic Sea; DEPTH, sediment/rock; Gravity corer (Kiel type); Greyscale value; IOW211610-3; KOT99/97/02.1; Multi-Sensor Core Logger/colorscan/scion image; Petr Kottsov; SL
    Type: Dataset
    Format: text/tab-separated-values, 65063 data points
    Location Call Number Limitation Availability
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  • 8
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    Unknown
    PANGAEA
    In:  Leibniz Institute for Baltic Sea Research, Warnemünde
    Publication Date: 2024-06-26
    Keywords: Baltic Sea System Study; BASYS; Bornholm Basin, Baltic Sea; DEPTH, sediment/rock; Gravity corer (Kiel type); Greyscale value; IOW211620-2; KOT99/97/02.1; Multi-Sensor Core Logger/colorscan/scion image; Petr Kottsov; SL
    Type: Dataset
    Format: text/tab-separated-values, 51809 data points
    Location Call Number Limitation Availability
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    PANGAEA
    In:  Leibniz Institute for Baltic Sea Research, Warnemünde
    Publication Date: 2024-06-26
    Keywords: Baltic Sea System Study; BASYS; DEPTH, sediment/rock; Gotland Basin, Baltic Sea; Gravity corer (Kiel type); Greyscale value; Gulf of Riga; IOW211640-7; KOT99/97/02.1; Multi-Sensor Core Logger/colorscan/scion image; Petr Kottsov; SL
    Type: Dataset
    Format: text/tab-separated-values, 81517 data points
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    PANGAEA
    In:  Leibniz Institute for Baltic Sea Research, Warnemünde
    Publication Date: 2024-06-26
    Keywords: Baltic Sea System Study; BASYS; DEPTH, sediment/rock; Gotland Basin, Baltic Sea; Gravity corer (Kiel type); Greyscale value; Gulf of Riga; IOW211650-5; KOT99/97/02.1; Multi-Sensor Core Logger/colorscan/scion image; Petr Kottsov; SL
    Type: Dataset
    Format: text/tab-separated-values, 55389 data points
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