@article{RutschkeNaacke1995, author = {Rutschke, Erich and Naacke, Johannes}, title = {Zur Situation der Wildg{\"a}nse in Ostdeutschland : Bestandsentwicklung seit 1990 ; Bestand 1994/95 ; Probleme.}, year = {1995}, language = {de} } @article{Knoesche1995, author = {Kn{\"o}sche, R{\"u}diger}, title = {Zur Rolle der Sedimente in verschiedenen Gew{\"a}ssern der Unteren Havel}, year = {1995}, language = {de} } @article{Naacke1999, author = {Naacke, Johannes}, title = {Zur Rolle der Jagd in RAMSAR-Gebieten}, year = {1999}, language = {de} } @article{ErlacherTrusch1999, author = {Erlacher, S.-I. and Trusch, Robert}, title = {Zur Phylogenie und Verbreitung der Arten der Dyscia-conspersaria ([Denis \& Schifferm{\"u}ller] 1775)-Gruppe (= Dyscia s.str.) (Lepidoptera: Geometridae)}, year = {1999}, language = {de} } @article{BurkartPrasse1996, author = {Burkart, Michael and Prasse, R{\"u}diger}, title = {Zur pflanzlichen Besiedlung wechselnasser Pionierstandorte im Elbhavelwinkel}, year = {1996}, language = {de} } @article{SchulzMuehleWilke1999, author = {Schulz, R. and M{\"u}hle, Ralf-Udo and Wilke, Thomas}, title = {Zur Odonatenfauna des einstweilig gesicherten Teichgebietes Lakoma}, year = {1999}, language = {de} } @article{SteinAltenbergerKreher2001, author = {Stein, Eckehard and Altenberger, Uwe and Kreher, Birgit}, title = {Zur Geologie des kristallinen Odenwaldes : seine magmatische und metamorphe Entwicklung}, year = {2001}, language = {de} } @phdthesis{Althaus1999, author = {Althaus, Tilmann}, title = {Zur Geochemie der Edelgase ultramafischer Mantelxenolithe und Alkalibasalte der Persani-Berge, Transsilvanien, Rum{\"a}nien}, address = {Potsdam}, pages = {V, 129, A1 - C10 S. : graph. Darst.}, year = {1999}, language = {de} } @article{BurkartPoetsch1996, author = {Burkart, Michael and P{\"o}tsch, Joachim}, title = {Zur floristischen Gliederung und Syntaxonomie der Brenndoldenwiesen in der Unteren Havelaue}, year = {1996}, language = {de} } @article{GelbrechtRoedelTrusch1998, author = {Gelbrecht, J{\"o}rg and R{\"o}del, Ingolf and Trusch, Robert}, title = {Zur Faunistik und {\"O}kologie der Schmetterlinge in der Mark Brandenburg, VX : aktuelle Verbreitung und {\"o}kologische Anspr{\"u}che von Scotopteryx coarctaria ([DENIS \& Schifferm{\"u}ller] 1775) in der Mark Brandenburg und den s{\"u}dlich angrenzenden Gebieten}, year = {1998}, language = {de} } @article{GelbrechtSbieschnieRoedeletal.1997, author = {Gelbrecht, J{\"o}rg and Sbieschnie, H. and R{\"o}del, Ingolf and Trusch, Robert}, title = {Zur Faunistik und {\"O}kologie der Schmetterlinge in der Mark Brandenburg, VIII : Aktuelle Verbreitung und {\"o}kologische Anspr{\"u}che von Selidosema brunnearia (VILLERS, 1789) in der Mark Brandenburg und in der angrenzenden Oberlausitz (Lepidoptera, Geometridae)}, year = {1997}, language = {de} } @article{RoedelTrusch1997, author = {R{\"o}del, Ingolf and Trusch, Robert}, title = {Zur Biologie, {\"O}kologie und Verbreitung von Biochroma famula (Esper, 1787) in Deutschland (Lepidoptera, Geometridae)}, year = {1997}, language = {de} } @article{Rutschke1994, author = {Rutschke, Erich}, title = {Zur Bedeutung von Rast-und Sammelpl{\"a}tzen f{\"u}r Verhalten und Schutz von Wasserv{\"o}geln nach Untersuchungen an Graug{\"a}nsen}, year = {1994}, language = {de} } @article{EllmannKnoescheRowinskyetal.1995, author = {Ellmann, H. and Kn{\"o}sche, R{\"u}diger and Rowinsky, V. and Rutter, S.}, title = {Zum {\"o}kologischen Zustand des Schollener Sees}, year = {1995}, language = {de} } @article{WallschlaegerBrehme1999, author = {Wallschl{\"a}ger, Hans-Dieter and Brehme, Angelika}, title = {Zum Verhalten von Kolkraben (Corvus corax) in Mutterkuh-Herden}, year = {1999}, language = {de} } @article{Rutschke1994, author = {Rutschke, Erich}, title = {Zum Problem der Artreinheit bei der Stockente Anas plathyrhynchos}, year = {1994}, language = {de} } @article{Rutschke1995, author = {Rutschke, Erich}, title = {Zum Problem der Artreinheit bei der Stockente}, year = {1995}, language = {de} } @article{Rutschke1997, author = {Rutschke, Erich}, title = {Zum Management von Ramsargebieten unter besonderer Ber{\"u}cksichtigung der Jagd}, year = {1997}, language = {de} } @article{PaascheTronickeDietrich2012, author = {Paasche, Hendrik and Tronicke, Jens and Dietrich, Peter}, title = {Zonal cooperative inversion of partially co-located data sets constrained by structural a priori information}, series = {Near surface geophysics}, volume = {10}, journal = {Near surface geophysics}, number = {2}, publisher = {European Association of Geoscientists \& Engineers}, address = {Houten}, issn = {1569-4445}, doi = {10.3997/1873-0604.2011033}, pages = {103 -- 116}, year = {2012}, abstract = {In many near-surface geophysical studies it is now common practice to collect co-located disparate geophysical data sets to explore subsurface structures. Reconstruction of physical parameter distributions underlying the available geophysical data sets usually requires the use of tomographic reconstruction techniques. To improve the quality of the obtained models, the information content of all data sets should be considered during the model generation process, e.g., by employing joint or cooperative inversion approaches. Here, we extend the zonal cooperative inversion methodology based on fuzzy c-means cluster analysis and conventional single-input data set inversion algorithms for the cooperative inversion of data sets with partially co-located model areas. This is done by considering recent developments in fuzzy c-means cluster analysis. Additionally, we show how supplementary a priori information can be incorporated in an automated fashion into the zonal cooperative inversion approach to further constrain the inversion. The only requirement is that this a priori information can be expressed numerically; e.g., by physical parameters or indicator variables. We demonstrate the applicability of the modified zonal cooperative inversion approach using synthetic and field data examples. In these examples, we cooperatively invert S- and P-wave traveltime data sets with partially co-located model areas using water saturation information expressed by indicator variables as additional a priori information. The approach results in a zoned multi-parameter model, which is consistent with all available information given to the zonal cooperative inversion and outlines the major subsurface units. In our field example, we further compare the obtained zonal model to sparsely available borehole and direct-push logs. This comparison provides further confidence in our zonal cooperative inversion model because the borehole and direct-push logs indicate a similar zonation.}, language = {en} } @article{KroenerWildeZhaoetal.2006, author = {Kr{\"o}ner, Alfred and Wilde, Simon A. and Zhao, Guochun and O'Brien, Patrick J. and Sun, Min and Liu, Dun Yi and Wan, Yusheng and Liu, S. W. and Guo, Jianbin H.}, title = {Zircon geochronology and metamorphic evolution of mafic dykes in the Hengshan Complex of northern China: Evidence for late Palaeoproterozoic extension and subsequent high-pressure metamorphism in the North China Craton}, issn = {0301-9268}, doi = {10.1016/j.precamres.2006.01.008}, year = {2006}, abstract = {Magmatic and metamorphic zircons have been dated from ductilely deformed gabbroic dykes defining a dyke swarm and signifying crustal extension in the northern part of the Hengshan Complex of the North China Craton, These dykes now occur as boudins and deformed sheets within migmatitic tonalitic, trondhjemitic, granodioritic and granitic gneisses and are conspicuous due to relics of high-pressure granulite or even former eclogite facies garnet + pyroxene-bearing assemblages. SHRIMP ages for magmatic zircons from two dykes reflect the time of dyke emplacement at similar to 1915 Ma, whereas metamorphic zircons dated by both SHRIMP and evaporation techniques are consistently in the range 1848-1888 Ma. The Youngest granitoid gneiss yet dated in the Hengshan has an emplacement age of 18 2 17 Ma. These results complement recent geochronological studies from the neighbouring Wutai and Fuping Complexes, to the SE of the Hengshan, showing that a crustal extension event Occurred in the late Palaeoproterozoic. This preceded a major high-pressure collision- type metamorphic event in the central part of the North China Craton that occurred in the Palaeoproterozoic and not in the late Archaean as previously thought. Our data support recent suggestions that the North China Craton experienced a major, craton-wide orogenic event in the late Palaeoproterozoic after which it became cratonized and acted as a stable block.}, language = {en} }