@inproceedings{Lueck2006,
  author    = {L{\"u}ck, Erika},
  title     = {Geophysik f{\"u}r den oberfl{\"a}chennahen Bereich (Landwirtschaft, Bodenkunde, Arch{\"a}ologie, Umwelt usw.)},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-7045},
  year      = {2006},
  abstract  = {Dokument 1: Foliensatz | Dokument 2: Animation <hr> Interdisziplin{\"a}res Zentrum f{\"u}r Musterdynamik und Angewandte Fernerkundung Workshop vom 9. - 10. Februar 2006},
  language  = {de}
}
@inproceedings{RehakStreckerEchtler2006,
  author    = {Rehak, Katrin and Strecker, Manfred and Echtler, Helmut Peter},
  title     = {DEM supported tectonic geomorphology : the Coastal Cordillera of the South-Central Chilean active margin ; [Poster]},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus-7224},
  year      = {2006},
  abstract  = {Fluvial systems are one of the major features shaping a landscape. They adjust to the prevailing tectonic and climatic setting and therefore are very sensitive markers of changes in these systems. If their response to tectonic and climatic forcing is quantified and if the climatic signal is excluded, it is possible to derive a local deformation history. Here, we investigate fluvial terraces and erosional surfaces in the southern Chilean forearc to assess a long-term geomorphic and hence tectonic evolution. Remote sensing and field studies of the Nahuelbuta Range show that the long-term deformation of the Chilean forearc is manifested by breaks in topography, sequences of differentially uplifted marine, alluvial and strath terraces as well as tectonically modified river courses and drainage basins. We used SRTM-90-data as basic elevation information for extracting and delineating drainage networks. We calculated hypsometric curves as an indicator for basin uplift, stream-length gradient indices to identify stream segments with anomalous slopes, and longitudinal river profiles as well as DS-plots to identify knickpoints and other anomalies. In addition, we investigated topography with elevation-slope graphs, profiles, and DEMs to reveal erosional surfaces. During the first field trip we already measured palaeoflow directions, performed pebble counting and sampled the fluvial terraces in order to apply cosmogenic nuclide dating (<sup>10Be, <sup>26Al) as well as provenance analyses. Our preliminary analysis of the Coastal Cordillera indicates a clear segmentation between the northern and southern parts of the Nahuelbuta Range. The Lanalhue Fault, a NW-SE striking fault zone oblique to the plate boundary, defines the segment boundary. Furthermore, we find a complex drainage re-organisation including a drainage reversal and wind gap on the divide between the Tir{\´u}a and Pellahu{\´e}n basins east of the town Tir{\´u}a. The coastal basins lost most of their Andean sediment supply areas that existed in Tertiary and in part during early Pleistocene time. Between the B{\´i}o-B{\´i}o and Imperial rivers no Andean river is recently capable to traverse the Coastal Cordillera, suggesting ongoing Quaternary uplift of the entire range. From the spatial distribution of geomorphic surfaces in this region two uplift signals may be derived: (1) a long-term differential uplift process, active since the Miocene and possibly caused by underplating of subducted trench sediments, (2) a younger, local uplift affecting only the northern part of the Nahuelbuta Range that may be caused by the interaction of the forearc with the subduction of the Mocha Fracture Zone at the latitude of the Arauco peninsula. Our approach thus provides results in our attempt to decipher the characteristics of forearc development of active convergent margins using long-term geomorphic indicators. Furthermore, it is expected that our ongoing assessment will constrain repeatedly active zones of deformation. <hr> Interdisziplin{\"a}res Zentrum f{\"u}r Musterdynamik und Angewandte Fernerkundung Workshop vom 9. - 10. Februar 2006},
  language  = {en}
}
@inproceedings{OPUS4-41661,
  title     = {International Conference on "Natural Hazards and Risks in a Changing World"},
  series = {Book of Abstracts},
  booktitle = {Book of Abstracts},
  editor    = {Petrow, Theresia and Bronstert, Axel and Thieken, Annegret and Vogel, Kristin},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-416613},
  pages     = {118},
  year      = {2018},
  abstract  = {Natural hazards such as floods, earthquakes, landslides, and multi-hazard events heavily affect human societies and call for better management strategies. Due to the severity of such events, it is of utmost importance to understand whether and how they change in re-sponse to evolving hydro-climatological, geo-physical and socio-economic conditions. These conditions jointly determine the magnitude, frequency, and impact of disasters, and are changing in response to climate change and human behavior. Therefore methods are need-ed for hazard and risk quantification accounting for the transient nature of hazards and risks in response to changing natural and anthropogenic altered systems. The purpose of this conference is to bring together researchers from natural sciences (e.g. hydrology, meteorology, geomorphology, hydraulic engineering, environmental science, seismology, geography), risk research, nonlinear systems dynamics, and applied mathematics to discuss new insights and developments about data science, changing systems, multi-hazard events and the linkage between hazard and vulnerabilities under unstable environmental conditions. Knowledge transfer, communication and networking will be key issues of the conference. The conference is organized by means of invited talks given by outstanding experts, oral presentations, poster sessions and discussions.},
  language  = {en}
}
@inproceedings{OPUS4-43269,
  title     = {RAA2019},
  editor    = {Ziemann, Martin Andreas},
  organization    = {University of Potsdam, Institute of Geosciences},
  doi       = {10.25932/publishup-43269},
  url       = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-432692},
  pages     = {149},
  year      = {2019},
  abstract  = {These abstracts result from the 10th International Congress on the Application of Raman Spectroscopy in Art and Archaeology held 03.09. - 07.09.2019 in Potsdam (Germany). The RAA is an established biennial international conference series. Since the beginning in 2001, the RAA conferences promote Raman Spectroscopy and play an important role in increasing the field of its applications in art history, history, archaeology, palaeontology, conservation and restoration, museology, degradation of cultural heritage, archaeometry, etc. Furthermore, the development of new instrumentation, especially for non-invasive measurements, receives great attention. The Congress covers all topics of Raman spectroscopic applications in art and archaeology and focuses on the following themes: • Material characterization and degradation processes • Conservation issues affecting cultural heritage • Raman spectroscopy of biological and organic materials • Surface enhanced Raman spectroscopy • Chemometrics in Raman spectroscopy • Development of Raman techniques • New Raman instrumentation and applications in cultural heritage objects investigations • Raman spectroscopy in paleontology, paleoenvironment and archaeology},
  language  = {en}
}