Paul, Josef

[["dc.bibliographiccitation.firstpage","95"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Zeitschrift der Deutschen Gesellschaft für Geowissenschaften"],["dc.bibliographiccitation.lastpage","107"],["dc.bibliographiccitation.volume","170"],["dc.contributor.author","Paul, Josef"],["dc.date.accessioned","2020-12-10T18:36:50Z"],["dc.date.available","2020-12-10T18:36:50Z"],["dc.date.issued","2019"],["dc.identifier.doi","10.1127/zdgg/2019/0181"],["dc.identifier.issn","1860-1804"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/76753"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Hat sich der Harz im jüngeren Tertiär und Quartär gehoben?"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","237"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Zeitschrift der Deutschen Gesellschaft für Geowissenschaften"],["dc.bibliographiccitation.lastpage","250"],["dc.bibliographiccitation.volume","173"],["dc.contributor.author","Paul, Josef"],["dc.date.accessioned","2022-06-01T09:39:35Z"],["dc.date.available","2022-06-01T09:39:35Z"],["dc.date.issued","2022"],["dc.identifier.doi","10.1127/zdgg/2021/0291"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/108512"],["dc.language.iso","en"],["dc.notes.intern","DOI-Import GROB-572"],["dc.relation.issn","1860-1804"],["dc.title","Palaeogeography and subrosion of the Werra Salt in the Hessian Depression, Zechstein, Germany."],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","139"],["dc.bibliographiccitation.issue","2"],["dc.bibliographiccitation.journal","Zeitschrift der Deutschen Gesellschaft für Geowissenschaften"],["dc.bibliographiccitation.lastpage","145"],["dc.bibliographiccitation.volume","169"],["dc.contributor.author","Paul, Josef"],["dc.contributor.author","Heggemann, Heiner"],["dc.contributor.author","Dittrich, Doris"],["dc.contributor.author","Hug-Diegel, Nicola"],["dc.contributor.author","Huckriede, Hermann"],["dc.contributor.author","Nitsch, Edgar"],["dc.contributor.authorgroup","AG Zechstein der SKPT/DSK"],["dc.date.accessioned","2020-12-10T18:36:49Z"],["dc.date.available","2020-12-10T18:36:49Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1127/zdgg/2018/0136"],["dc.identifier.issn","1860-1804"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/76749"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","Erläuterungen zur Stratigraphischen Tabelle von Deutschland 2016: die Zechstein-Gruppe"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Scientific Reports"],["dc.bibliographiccitation.volume","8"],["dc.contributor.author","Batchelor, Murray T."],["dc.contributor.author","Burne, Robert V."],["dc.contributor.author","Henry, Bruce I."],["dc.contributor.author","Li, Fei"],["dc.contributor.author","Paul, Josef"],["dc.date.accessioned","2020-12-10T18:10:08Z"],["dc.date.available","2020-12-10T18:10:08Z"],["dc.date.issued","2018"],["dc.identifier.doi","10.1038/s41598-017-18908-4"],["dc.identifier.eissn","2045-2322"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/73860"],["dc.language.iso","en"],["dc.notes.intern","DOI Import GROB-354"],["dc.title","A biofilm and organomineralisation model for the growth and limiting size of ooids"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","110"],["dc.bibliographiccitation.issue","1-2"],["dc.bibliographiccitation.journal","Palaeogeography Palaeoclimatology Palaeoecology"],["dc.bibliographiccitation.lastpage","125"],["dc.bibliographiccitation.volume","242"],["dc.contributor.author","Quast, Andres"],["dc.contributor.author","Hoefs, Jochen"],["dc.contributor.author","Paul, Josef"],["dc.date.accessioned","2018-11-07T08:57:04Z"],["dc.date.available","2018-11-07T08:57:04Z"],["dc.date.issued","2006"],["dc.description.abstract","According to a model by Cerling [Cerling, T. E., 1991. Carbon dioxide in the paleoatmosphere: evidence from Cenozoic and Mesozoic paleosols. Am. J. Sci. 291, 377-400, Cerling, T. E., 1999. Stable carbon isotopes in palaeosol carbonates. In: Thiry, M., Simon-Coincon, R. (Eds.), Palaeoweathering, Palaeosurfaces and Related Continental Deposits. vol. 27 of Spec. Publ. Int. Assoc. Sediment., pp. 43-60], the carbon isotope composition of calcretes should depend on the soil type and the CO2-concentration in the atmosphere. We have tested Cerling's model by investigating 14 Palaeozoic sections with soil profiles. A large number of carbonate types of different genetic origin exist in the localities examined. Comparing the Palaeozoic samples with recent and subrecent calcretes, it can be demonstrated that anhedral, cryptocrystalline (< 10 mu m) and subhedral microcrystalline (10-40 mu m) carbonates are clearly of pedogenic origin. Crystals of larger size with a poikilotopic texture are of groundwater or burial diagenetic origin. Macro- and micromorphological features, typical of recent calcretes, occur in several soil profiles, but thin section microscopy reveals a strong diagenetic overprint of most pedogenic carbonates. Time equivalent sections with comparable soil types (protosols, calcisols and vertisols) show large variations in carbon isotope composition. On the other hand, different carbonate generations at one site do not differ much. Therefore Palaeozoic calcretes appear to be unsuitable for a deduction of the Palaeozoic CO2-concentration. (c) 2006 Elsevier B.V All rights reserved."],["dc.identifier.doi","10.1016/j.palaeo.2006.05.017"],["dc.identifier.isi","000242463400007"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/23302"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Elsevier Science Bv"],["dc.relation.issn","0031-0182"],["dc.title","Pedogenic carbonates as a proxy for palaeo-CO2 in the Palaeozoic atmosphere"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","69"],["dc.bibliographiccitation.lastpage","78"],["dc.contributor.author","Ziesch, Jennifer"],["dc.contributor.author","Tanner, David C."],["dc.contributor.author","Arp, Gernot"],["dc.contributor.author","Paul, Josef"],["dc.contributor.editor","Leiss, Bernd"],["dc.contributor.editor","Tanner, David"],["dc.contributor.editor","Vollbrecht, Axel"],["dc.contributor.editor","Arp, Gernot"],["dc.date.accessioned","2020-05-04T11:30:31Z"],["dc.date.available","2020-05-04T11:30:31Z"],["dc.date.issued","2011"],["dc.description.abstract","Im Rahmen von verschiedenen Geothermie-Projekten wurden im östlichen Stadtgebiet von Göttingen Bohrungen beprobt, analysiert und beschrieben. Die Bohrung 2 (Tannenweg 20) durchteufte dabei die hier unter der Lias-Gruppe liegende, östliche Grabenrandstörung und traf auf Gipse des Mittleren Muschelkalkes. Für einen Aufstieg von Zechstein-Evaporiten entlang der Grabenrandstörung, so wie vormals vermutet, finden sich damit keine Belege. Unter Einbindung von weiteren Bohrungen und Fundstücken aus dem Museum des GZG sowie Fundangaben aus geologischen Kartierungen des frühen 19. Jahrhunderts hat sich der Verlauf der östlichen Grabenrandstörung gegenüber der publizierten Karte von Stille (1932) um etwa 100m in Richtung Osten verschoben. Weiterhin zeigte sich in der erstellten, geologischen Karte, dass eine dextrale Seitenverschiebung eine Umbiegung der Lias-Schichten im Norden und einen dextralen Versatz der östlichen Grabenrandstörung von etwa 70m verursacht. Das generierte, strukturgeologische 3D-Modell zeigt, dass die Basis der als Leithorizont genutzten Lias-γ-Kalksteinbank im n¨ordlichen Bereich einen ausgeprägten Knick aufweist und mit 30°steiler als der südliche Bereich einfällt. Ferner konnte anhand der 3D-Modellierung die Orientierung der östlichen Grabenrandstörung mit 289/55 ermittelt werden. Abstract— Within the context of various geothermal projects, wells were sampled, analysed and described from the eastern side of the city of G¨ ottingen. The well No. 2 (Tannenweg 20) encountered, in addition to the Lower Jurassic Lias Formation, the eastern Leinetal border fault and then gypsum layers of the Middle Muschelkalk. The previous assumption that Zechstein had risen along the border faults, could not be confirmed in this work. With the information from wells and finds from the museum of the GZG, and geological maps and their memoirs from the early 19th Century, the trace of the main eastern border fault was moved about 100 metres toward the east. From the resulting geological map it becomes apparent that a dextral strike-slip fault caused a bend in the Liassic strata to the north and a dextral displacement of the eastern border fault by ca. 70 metres. The generated 3D structural geological model indicates that the base of Lias γ horizon in the northern area has a pronounced bend and dips 30°steeper than the southern area. By the use of 3D modelling, it was possible to determine that the orientation of the eastern border fault in this area is 289/55."],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/64595"],["dc.language.iso","de"],["dc.publisher","Universitätsverlag Göttingen"],["dc.publisher.place","Göttingen"],["dc.relation.ispartof","Neue Untersuchungen zur Geologie der Leinetalgrabenstruktu"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Strukturgeologische 3D-Modellierung der Grabenrandstörung des Leinetals im östlichen Stadtgebiet von Göttingen"],["dc.type","book_chapter"],["dc.type.internalPublication","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","116"],["dc.bibliographiccitation.issue","0"],["dc.bibliographiccitation.journal","Geotectonic Research"],["dc.bibliographiccitation.lastpage","118"],["dc.bibliographiccitation.volume","95"],["dc.contributor.author","Michler, Alexander"],["dc.contributor.author","Leiss, Bernd"],["dc.contributor.author","Tanner, David Colin"],["dc.contributor.author","Paul, Josef"],["dc.contributor.author","Arp, Gernot"],["dc.date.accessioned","2020-05-04T11:31:36Z"],["dc.date.available","2020-05-04T11:31:36Z"],["dc.date.issued","2008"],["dc.description.abstract","Im Leinetalgraben in Sudniedersachsen wurden im Bereich des ostlichen, N-S streichenden GrabenrandstOnmgssystems stratigraphische und strukturelle Detailaufuahmen im Keuper durchgefiihrt. Das generelle Einfallen der Keuperschichten mit ca. 25° gegen die GrabenrandstOrung weist auf ein listrisches StOrungssystem hin. Neben einer nachweisbaren NW-SE streichenden StOrung, muss aus den Schichtmachtigkeitsverhaltnissen auf weitere grabenrandparallele Abschiebungen geschlossen werden. Diese Ergebnisse gehen in die Planung und spatere Interpretation eines seismsichen Profils in diesem Bereich ein."],["dc.identifier.doi","10.1127/1864-5658/08/9501-0116"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/64603"],["dc.language.iso","de"],["dc.relation.issn","1864-5658"],["dc.relation.orgunit","Abteilung Strukturgeologie und Geodynamik"],["dc.title","Detailuntersuchungen zur Tektonik am ostlichen Rand der Leinetalgrabenstruktur bei Bovenden, Sudniedersachsen"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.subtype","original_ja"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","1"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Zeitschrift der Deutschen Gesellschaft für Geowissenschaften"],["dc.bibliographiccitation.lastpage","18"],["dc.bibliographiccitation.volume","162"],["dc.contributor.author","Menning, Manfred"],["dc.contributor.author","Schroeder, Bernt"],["dc.contributor.author","Plein, Eberhard"],["dc.contributor.author","Simon, Theo"],["dc.contributor.author","Lepper, Jochen"],["dc.contributor.author","Roehling, Heinz-Gerd"],["dc.contributor.author","Heunisch, Carmen"],["dc.contributor.author","Stapf, Karl"],["dc.contributor.author","Luetzner, Harald"],["dc.contributor.author","Kaeding, Karl-Christian"],["dc.contributor.author","Paul, Josef"],["dc.contributor.author","Horn, Manfred"],["dc.contributor.author","Hagdorn, Hans"],["dc.contributor.author","Beutler, Gerhard"],["dc.contributor.author","Nitsch, Edgar"],["dc.date.accessioned","2018-11-07T08:58:36Z"],["dc.date.available","2018-11-07T08:58:36Z"],["dc.date.issued","2011"],["dc.description.abstract","After the re-unification of Germany on October 3rd 1990, the \"Subkommission Perm-Trias\" (SKPT) of the German Stratigraphic Commission passed recommendations on 70 applications concerning stratigraphic nomenclature, classification (rank), subdivision of stratigraphic units and items of procedure in Central Europe. Here, the most important 33 of these recommendations are documented, with some additional explanations. A full list of recommendations can be found on the website www.stratigraphie.de/Perm-Trias. The stratigraphic systems of the Federal Republic of Germany and the German Democratic Republic differed significantly and they have now been aligned with each other and with the International Stratigraphic Guide (ISG 1976, 1994). The 33 resolutions given here are listed in five groups by ascending stratigraphic order - Rotliegend, Zechstein, Buntsandstein, Muschelkalk and Keuper - irrespective of when the resolutions were passed. For each unit, the listings include the lower boundary, rank (classification), subdivisions and the results of the voting. Figures are provided to illustrate the position and rank of the stratigraphic units mentioned. After a final resolution fixing the lower boundary of the Rotliegend in 2006, the two groups of the Dyas (Rotliegend and Zechstein = Central European Permian) and the three Germanic Trias groups (Buntsandstein, Muschelkalk and Keuper = Central European Triassic) are now firmly established. The boundaries between the five groups, and those separating the numerous formations within them, are quasi-iso-chronous across large parts of the Central European Basin (Germanic Basin). This is an extremely valuable geochronological component of the stratigraphy, and to make it fully accessible, the German Stratigraphic Commision has defined 33 \"Folgen\" (intervals) as \"regional geochronological units\" (RGU) after thorough discussions."],["dc.identifier.doi","10.1127/1860-1804/2011/0162-0001"],["dc.identifier.isi","000288319200001"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/23683"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","E Schweizerbartsche Verlags"],["dc.relation.issn","1860-1804"],["dc.title","The German Stratigraphic Commission recommends the use of the new stratigraphic classifications of the Permian and Triassic units of Germany"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","641"],["dc.bibliographiccitation.issue","4"],["dc.bibliographiccitation.journal","Zeitschrift der Deutschen Gesellschaft für Geowissenschaften"],["dc.bibliographiccitation.lastpage","650"],["dc.bibliographiccitation.volume","159"],["dc.contributor.author","Paul, Josef"],["dc.contributor.author","Wemmer, Klaus"],["dc.contributor.author","Ahrendt, Hans"],["dc.date.accessioned","2018-11-07T11:20:54Z"],["dc.date.available","2018-11-07T11:20:54Z"],["dc.date.issued","2008"],["dc.description.abstract","Isotopic cooling ages of detrital white micas arc used as markers for source ages and provenance of siliciclastic sediments in the Central European Basin. Zechstein deposits at the Southern margin of the basin were Supplied from the nearby Saxo-Thuringian Zone of the Variscan Orogen (340 Ma). Buntsandstein sediments originate from late Variscan rocks (310 Ma) of the Bohemian Massif, the Vindelician High or the French Massif Central, whereas detrital micas from the Middle Buntsandstein of the north German island of Helgoland have a Cadomian age (577 Ma). Provenance may be from Southern Poland or Czech Republic and Slovakia. Sandy Muschelkalk in southern Germany originates from the Bohemian and Vindelician Massifs. Source areas of Lower Keuper sediments and the Schilfsandstein (Stuttgart Fin.) are the Caledonides in western Norway (400 Ma). In contrast to this, the Fermoscandian Shield never delivered any material to western and southern Germany. In southern Germany, the terrigenous Keuper deposits above the Schilfsandstein consist of detritus from the Bohemian Massif (320 Ma). In northern Germany, the Upper Keuper siliciclastics are of Cadomian age (570 Ma) and are derived from Polish or Slovakian sources. Lias and Dogger detrital Muscovites in northern Germany are also of Cadomian age (555 665 Ma), whereas in southern Germany in the Lias Variscan material from the Bohemian Massif was deposited (350 Ma). Only Dogger micas yielded Cadomian ages (580 Ma)."],["dc.identifier.doi","10.1127/1860-1804/2008/0159-0641"],["dc.identifier.isi","000261786600005"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/55645"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.relation.issn","1860-1804"],["dc.title","Provenance of siliciclastic sediments (Permian to Jurassic) in the Central European Basin"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dspace.entity.type","Publication"]]

[["dc.bibliographiccitation.firstpage","45"],["dc.bibliographiccitation.issue","1"],["dc.bibliographiccitation.journal","Carbonates and Evaporites"],["dc.bibliographiccitation.lastpage","57"],["dc.bibliographiccitation.volume","24"],["dc.contributor.author","Kovalevych, Volodymyr"],["dc.contributor.author","Paul, Josef"],["dc.contributor.author","Peryt, Tadeusz Marek"],["dc.date.accessioned","2018-11-07T08:28:59Z"],["dc.date.available","2018-11-07T08:28:59Z"],["dc.date.issued","2009"],["dc.description.abstract","The study of fluid inclusions in Lower Triassic Rot halite from the Rockensussra 2/83 borehole in northern Germany showed the presence of primary and secondary gas-liquid inclusions. The gas phase in inclusions indicates their stretching due to salt overheating at some postsedimentary stage. The homogenization temperature of inclusions indicates the overheating temperature of about 60-70 degrees C. The overheating is additionally indicated by trails of migration of large secondary inclusions Occurring inside chevrons. The major-ion (K, Mg and SO4) composition of inclusion brines was established with the use of ultramicrochemical analysis (UMCA). The results of chemical analyses of brines of primary inclusions in halite from the Rockensussra 2/83 borehole confirm the earlier results for the Rot halite from the Netherlands and Poland. The bromine content in halite is 78-107 ppm, supporting thus marine origin of halite. Brines of primary gas-liquid inclusions are thus representative,e samples of trapped evaporite water and they may be used for the reconstruction of the composition of Early Triassic seawater. The comparison of our analytical data with the earlier published data and models of chemical composition of seawater during the Phanerozoic which were constructed with the use of the HMW computer program makes it possible to conclude that the Early Triassic seawater was of the SO4-rich type and considering the ratios of major ions it fully corresponded to the Early Permian (Asselian-Sakmarian) seawater. It differed from the present seawater by a slight decrease of Na and Mg ions, a considerable decrease of SO4 ion (by 31%) and an increase of Ca ion (by 36%)."],["dc.identifier.isi","000268357500004"],["dc.identifier.uri","https://resolver.sub.uni-goettingen.de/purl?gro-2/16545"],["dc.notes.status","zu prüfen"],["dc.notes.submitter","Najko"],["dc.publisher","Springer"],["dc.relation.issn","0891-2556"],["dc.title","FLUID INCLUSIONS IN HALITE FROM THE ROT (LOWER TRIASSIC) SALT DEPOSIT IN CENTRAL GERMANY: EVIDENCE FOR SEAWATER CHEMISTRY AND CONDITIONS OF SALT DEPOSITION AND RECRYSTALLIZATION"],["dc.type","journal_article"],["dc.type.internalPublication","yes"],["dc.type.peerReviewed","yes"],["dc.type.status","published"],["dspace.entity.type","Publication"]]