@book{BernerHoffmannMuehlbaueretal.2017, author = {Berner, Elisabeth and Hoffmann, Michael and M{\"u}hlbauer, Evelyn and H{\"o}fner, Marion and Weber, Carina and Giers, Ursula and Wiese, Heike and Freywald, Ulrike and Mayr, Katharina and Nowak, Měto and F{\"o}llner, Ursula and Luther, Saskia and Goltz, Reinhard}, title = {Region - Sprache - Literatur}, editor = {Berner, Elisabeth}, publisher = {Universit{\"a}tsverlag Potsdam}, address = {Potsdam}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-400098}, publisher = {Universit{\"a}t Potsdam}, year = {2017}, abstract = {Mit dem neuen Rahmenlehrplan f{\"u}r die L{\"a}nder Brandenburg und Berlin wird der Kompetenzentwicklung der Sch{\"u}lerinnen und Sch{\"u}ler unter den Bedingungen lebensweltlicher Erfahrungen ein besonderer Stellenwert beigemessen. Der Sammelband enth{\"a}lt Beitr{\"a}ge, in denen den Lehrerinnen und Lehrern vielf{\"a}ltige Unterrichtsmaterialien und didaktische Anregungen f{\"u}r einen praxisnahen, entdeckenden Unterricht in der Primar- und Sekundarstufe f{\"u}r den Deutschunterricht vorgestellt werden. Diese reichen von theoretischen Grundlagen, {\"u}ber einzelne Unterrichtssequenzen und Projekte bis zur Darstellung einer Lernspirale f{\"u}r die Jahrgangsstufen 1 bis 10. Vielf{\"a}ltige, auch multimediale Zug{\"a}nge bis zum spielerischen Umgang mit der Sprache zeigen, dass Sprache kein „trockener" Lerngegenstand sein muss. Die Beitr{\"a}ge geben dar{\"u}ber hinaus Einblicke in die fachlichen Hintergr{\"u}nde, die helfen sollen, den Zugang zu den einzelnen Gegenst{\"a}nden zu erleichtern. Das thematische Zentrum „Region" bildet den Ausgangspunkt f{\"u}r die Einbeziehung des Niederdeutschen, Sorbischen, Berlinischen, Kiezdeutschen sowie der Dialekte. Dabei werden sowohl literarische als auch Sachtexte ber{\"u}cksichtigt.}, language = {de} } @article{HoefnerWeber2017, author = {H{\"o}fner, Marion and Weber, Carina}, title = {Literarische Spurensuche}, series = {Region - Sprache - Literatur}, journal = {Region - Sprache - Literatur}, publisher = {Universit{\"a}tsverlag Potsdam}, address = {Potsdam}, url = {http://nbn-resolving.de/urn:nbn:de:kobv:517-opus4-403015}, pages = {43 -- 75}, year = {2017}, language = {de} } @article{WeberCardonaValenciaetal.2011, author = {Weber, Marion and Cardona, A. and Valencia, V. and Altenberger, Uwe and Lopez-Martinez, M. and Tobon, M. and Zapata, Sebastian Henao and Zapata, G. and Concha, A. E.}, title = {Geochemistry and geochronology of the Guajira Eclogites, northern Colombia evidence of a metamorphosed primitive Cretaceous Caribbean Island-arc}, series = {Geologica acta}, volume = {9}, journal = {Geologica acta}, number = {3-4}, publisher = {Facultat de Geologia, Divisio III, Ci{\`e}ncies Experimentals i Matem{\`a}tiques, Universitat de Barcelona}, address = {Barcelona}, issn = {1695-6133}, doi = {10.1344/105.000001740}, pages = {425 -- 443}, year = {2011}, abstract = {The chemical composition of eclogites, found as boulders in a Tertiary conglomerate from the Guajira Peninsula, Colombia suggests that these rocks are mainly metamorphosed basaltic andesites. They are depleted in LILE elements compared to MORB, have a negative Nb-anomaly and flat to enriched REE patterns, suggesting that their protoliths evolved in a subduction related tectonic setting. They show island-arc affinities and are similar to primitive island-arc rocks described in the Caribbean. The geochemical characteristics are comparable to low-grade greenschists from the nearby Etpana Terrane, which are interpreted as part of a Cretaceous intra-oceanic arc. These data support evidence that the eclogites and the Etpana terrane rocks formed from the same volcano-sedimentary sequence. Part of this sequence was accreted onto the margin and another was incorporated into the subduction channel and metamorphosed at eclogite facies conditions. Ar-40-Ar-39 ages of 79.2 +/- 1.1Ma and 82.2 +/- 2.5Ma determined on white micas, separated from two eclogite samples, are interpreted to be related to the cooling of the main metamorphic event. The formation of a common volcano-sedimentary protolith and subsequent metamorphism of these units record the ongoing Late Cretaceous continental subduction of the South American margin within the Caribbean intra-oceanic arc subduction zone. This gave way to an arc-continent collision between the Caribbean and the South American plates, where this sequence was exhumed after the Campanian.}, language = {en} }