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Auf dieser Seite finden Sie eine Sammlung von Links zu wissenschaftlichen Veröffentlichungen, die für dieses Projekt relevant sind oder die dazu beitragen können, ein tieferes exemplarisches Verständnis über die Prozesse und Umstände zu erlangen, welche möglicherweise in einem Zusammenhang mit der hier vorgestellten Neuinterpretation der Germania Magna stehen. Dabei handelt es sich um Veröffentlichungen unterschiedlicher Forschungsbereiche.
Die Sammlung umfasst:
- Primärliteratur: Wissenschaftliche Veröffentlichungen, die die Ergebnisse neuer Forschung präsentieren.
- Sekundärliteratur: Wissenschaftliche Veröffentlichungen, die die Primärliteratur zusammenfassen, analysieren oder interpretieren.
- Vergleichende Literatur: Veröffentlichungen, die Ihnen exemplarisch ähnliche Prozesse und Umstände in anderen Kontexten aufzeigen.
- Weitere Ressourcen: Links zu Websites, Datenbanken und anderen Ressourcen, die für die Neuinterpretation relevant sein können.
Die folgenden Publikationen sollen dabei helfen, bestimmte Fragestellungen exemplarisch zu beantworten, welche in einem möglichen Zusammenhang mit den notwendigen Prozessen und Vorgängen stehen, die für eine umfangreiche Landschaftstransformation erforderlich sind. Hierzu zählen beispielsweise Überlegungen über tektonische Bruchereignisse und Rift-Systeme, mit entsprechender Auswirkung auf maritime Rutschungsereignisse und die Entstehung neuer Sedimentationsbecken.
- Continental-scale temperature variability during the past two millennia
DOI https://doi.org/10.1038/ngeo1797 Abstract Past global climate changes had strong regional expression. To elucidate their spatio-temporal pattern, we reconstructed past temperatures for seven continental-scale regions during the past one to two millennia. The most coherent feature in nearly all of the regional temperature reconstructions is a long-term cooling trend, which ended late … WeiterlesenContinental-scale temperature variability during the past two millennia - Seismic velocity structure of crustal intrusions in the Danish BasinDOI 10.1016/j.tecto.2011.11.019 We image the east- and westward extent of a crustal high-velocity body, the thickness of a layered sequence around the Moho at the flank of the body, and the uppermost mantle velocity along the 320 km long refraction and wide-angle reflection seismic profile ESTRID 2007 in the Danish Basin. … WeiterlesenSeismic velocity structure of crustal intrusions in the Danish Basin
- Mechanism for the Uplift of Gongga Shan in the Southeastern Tibetan Plateau Constrained by 3D Magnetotelluric DataDOI http://dx.doi.org/10.1029/2021GL097394 Abstract Plain Language Summary Continent‐continent collisions are an important tectonic process and have controlled the formation of the modern continents. The India‐Asia collision is the best modern example and has produced both a high elevation plateau and the world’s highest mountain belts. A range of tectonic processes occurs during … WeiterlesenMechanism for the Uplift of Gongga Shan in the Southeastern Tibetan Plateau Constrained by 3D Magnetotelluric Data
- Dynamics of Mid-Palaeocene North Atlantic rifting linked with European intra-plate deformationsDOI https://doi.org/10.1038/nature06379 Abstract The process of continental break-up provides a large-scale experiment that can be used to test causal relations between plate tectonics and the dynamics of the Earth’s deep mantle1,2. Detailed diagnostic information on the timing and dynamics of such events, which are not resolved by plate kinematic reconstructions, can … WeiterlesenDynamics of Mid-Palaeocene North Atlantic rifting linked with European intra-plate deformations
- A submerged Stone Age hunting architecture from the Western Baltic SeaDOI https://doi.org/10.1073/pnas.2312008121 Abstract The Baltic Sea basins, some of which only submerged in the mid-Holocene, preserve Stone Age structures that did not survive on land. Yet, the discovery of these features is challenging and requires cross-disciplinary approaches between archeology and marine geosciences. Here, we combine shipborne and autonomousunderwater vehicle hydroacoustic data … WeiterlesenA submerged Stone Age hunting architecture from the Western Baltic Sea
- A new tectonic model for the Laurentia−Avalonia−Baltica sutures in the North Sea: A case study along MONA LISA profile 3DOI http://dx.doi.org/10.1016/j.tecto.2006.09.017 Abstract We present a new model for the lithospheric structure of the transitions between Laurentia, Avalonia and Baltica in the North Sea, northwestern Europe based on 2¾D potential field modelling of MONA LISA profile 3 across the Central Graben, with constraints from seismic P-wave velocity models and the crustal … WeiterlesenA new tectonic model for the Laurentia−Avalonia−Baltica sutures in the North Sea: A case study along MONA LISA profile 3
- Sea-level change, glacial rebound and mantle viscosity for northern EuropeKurt Lambeck, Catherine Smither, Paul Johnston, Sea-level change, glacial rebound and mantle viscosity for northern Europe, Geophysical Journal International, Volume 134, Issue 1, July 1998, Pages 102–144
- Continuous record of Holocene sea-level changes and coastal development of the Kattegat island Læsø (4900 years BP to present)DOI http://dx.doi.org/10.37570/bgsd-2016-64-01 Læsø is the largest island of the Kattegat–Skagerrak region and exposes a vast array of relative sealevel (RSL) indicators, mainly raised beach ridges, swales, lagoons and saltmarshes. The physical environment of continuous glacial rebound, excessive supply of sediment, shallow surrounding waters, low amplitudes of near-shore waves, and micro-tidal conditions … WeiterlesenContinuous record of Holocene sea-level changes and coastal development of the Kattegat island Læsø (4900 years BP to present)
- Holocene Relative Sea-Level Changes from Near-, Intermediate-, and Far-Field LocationsDOI https://dx.doi.org/10.1007/s40641-015-0029-z Abstract Holocene relative sea-level (RSL) records exhibit spatial and temporal variability that arises mainly from the interaction of eustatic (land ice volume and thermal expansion) and isostatic (glacio- and hydro-) factors. We fit RSL histories from near-, intermediate-, and far-field locations with noisy-input Gaussian process models to assess rates … WeiterlesenHolocene Relative Sea-Level Changes from Near-, Intermediate-, and Far-Field Locations
- Abrupt Holocene ice loss due to thinning and ungrounding in the Weddell Sea Embayment. Nature GeoscienceDOI https://doi.org/10.1038/s41561-024-01375-8 Abstract The extent of grounded ice and buttressing by the Ronne Ice Shelf, which provides resistance to the outflow of ice streams, moderate West Antarctic Ice Sheet stability. During the Last Glacial Maximum, the ice sheet advanced and was grounded near the Weddell Sea continental shelf break. The timing … WeiterlesenAbrupt Holocene ice loss due to thinning and ungrounding in the Weddell Sea Embayment. Nature Geoscience
- One Thousand Centuries of Climatic Record from Camp Century on the Greenland Ice SheetDOI http://dx.doi.org/10.1126/science.166.3903.377 Abstract A correlation of time with depth has been evaluated for the Camp Century, Greenland, 1390 meter deep ice core. Oxygen isotopes in approximately 1600 samples throughout the core have been analyzed. Long-term variations in the isotopic composition of the ice reflect the climatic changes during the past nearly … WeiterlesenOne Thousand Centuries of Climatic Record from Camp Century on the Greenland Ice Sheet
- The catastrophic final flooding of Doggerland by the Storegga Slide tsunamiDOI https://doi.org/10.4312/dp.35.1 Abstract Around 8200 calBP, large parts of the now submerged North Sea continental shelf (‘Doggerland’) were catastrophically flooded by the Storegga Slide tsunami, one of the largest tsunamis known for the Holocene, which was generated on the Norwegian coastal margin by a submarine landslide. In the present paper, we … WeiterlesenThe catastrophic final flooding of Doggerland by the Storegga Slide tsunami
- Rapid Quaternary subsidence in the northwestern German North SeaDOI https://doi.org/10.1038/s41598-018-29638-6 Abstract 3D and 2D seismic data reveal the base-reflection of the Quaternary in the northwestern German North Sea locally at depths of more than 1000 m. This indicates extremely fast subsidence, with a rate of up to 480 m/Ma during the Quaternary, resulting in a NNW-SSE oriented sedimentary depocentre. Distinct iceberg … WeiterlesenRapid Quaternary subsidence in the northwestern German North Sea
- The Thor suture zone: From subduction to intraplate basin settingDOI http://dx.doi.org/10.1130/G37958.1 Abstract The crustal seismic velocity structure of northwestern Europe shows a low P-wave velocity zone (LVZ) in the lower crust along the Caledonian Thor suture zone (TSZ) that cannot be easily attributed to Avalonia or Baltica plates abutting the TSZ. The LVZ appears to correspond to a hitherto unrecognized … WeiterlesenThe Thor suture zone: From subduction to intraplate basin setting
- Fault system evolution in the Baltic Sea area west of Rügen, NE GermanyDOI https://doi.org/10.1144/sp469.24 Abstract Based on reprocessed offshore seismic lines acquired during oil and gas exploration in the 1980s, we reconstruct the formation and reactivation of major fault systems in the southern Baltic Sea area since the late Paleozoic. The geological evolution of different crustal blocks from the Caledonian Avalonia-Baltica collision until … WeiterlesenFault system evolution in the Baltic Sea area west of Rügen, NE Germany
