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dc.contributor.authorArp, Gernot
dc.contributor.editorEynatten, H. von
dc.contributor.editorRuppert, H.
dc.contributor.editorDunkl, I.
dc.contributor.editorFischer, C.
dc.contributor.editorKarius, V.
dc.date.accessioned2010-11-24T15:58:23Z
dc.date.available2010-11-24T15:58:23Z
dc.date.issued2006-06
dc.identifier.citationSchriftenreihe der Deutschen Gesellschaft für Geowissenschaften
dc.identifier.citationEynatten, H. v., Dunkl, I., Fischer, C., Karius, V.; Ruppert, H. (eds.): Sediment 2006 - 21th meeting of sedimentologists ; 4th meeting of SEPM Central European Section ; June 6 - 11, 2006, Geowissenschaftliches Zentrum, Georg-August-Universität Göttingen, Germany ; abstracts and field trips; 2006, Deutsche Gesellschaft für Geowissenschaftten, Hannover
dc.identifier.isbn3-932537-41-6
dc.identifier.urihttp://hdl.handle.net/11858/00-1735-0000-0001-33C0-D
dc.description.abstractThe Nördlinger Ries is a circular, flat depression of 22-24 km diameter separating the Jurassic limestone plateaus of the Franconian and Swabian Alb in Southwest-Germany. Its centre is located 110 km NW of Munich, 70 km SSW of Nuremberg and 110 km E of Stuttgart. The Ries basin was formed approximately 15 Million years ago (Gentner & Wagner, 1969; Staudacher et al., 1982) by an impact of a stony meteorite less than 1 km in size (Shoemaker & Chao, 1961; Stöffler, 1977). The Ries crater represents one of the best preserved and best investigated impact structures on Earth (Bayerisches Geologisches Landesamt 1969, 1974, 1977; Hüttner & Schmidt-Kaler 1999; Stöffler & Ostertag 1983). It gained wide public attention (e.g., Metz 1974, Steinert 1974, Lemcke 1981, Kavasch 1985, Pösges & Schieber 1994; Schieber 2004) and served as training site for Apollo 17 astronauts in August 1970 (e.g., Margolin 2000). However, apart from its impact nature, the Ries basin offers a great opportunity to study fossil lacustrine microbialites. Such lacustrine deposits within impact structures are of increasing interest for understanding the origin and evolution of early life on Earth, and possibly other planets (Cockell & Lee 2002, Osinski et al. 2005, Cabrol et al. 2001). Therefore, the focus on this field trip is on microbial and algal build-ups, their facies context, and the discussion of microbial effects and lake water chemistry.
dc.format.mimetypeapplication/pdf
dc.language.isoeng
dc.publisherDteutsche Gesellschaft für Geowissenschaften, Hannover
dc.relation.ispartofSediment 2006 - 21th meeting of sedimentologists
dc.subject.ddc551
dc.subject.gokVKB 380
dc.subject.gokVEB 147
dc.subject.gokVDI 121
dc.subject.gokVKB 376
dc.subject.gokVAE 150
dc.titleField Trip F2: Sediments of the Ries Crater Lake (Miocene, Southern Germany)
dc.typearticle
dc.subject.gokverbalSedimente bestimmter Regionen
dc.subject.gokverbalSchwäbische Alb und Fränkische Alb {Geologie}
dc.subject.gokverbalMiozän
dc.subject.gokverbalOrganogene Sedimentgesteine
dc.subject.gokverbalStrukturelle Erscheinungen {Strukturgeologie}
dc.identifier.doi10.23689/fidgeo-1791
dc.subject.freeRies
dc.subject.freeGeologie
dc.subject.freeGeologie
dc.subject.freeSeesediment
dc.subject.freeBiogenes Sediment
dc.subject.bk38.44
dc.subject.bk38.28
dc.relation.collectionGeologische Wissenschaften
dc.description.typeexcursionguide


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