ALBERT

All Library Books, journals and Electronic Records Telegrafenberg

X
feed icon rss

Your email was sent successfully. Check your inbox.

An error occurred while sending the email. Please try again.

Proceed reservation?

Export
  • 1
    Series available for loan
    Series available for loan
    Jungpleistozäne Strandterrassen in Südost-Lakonien : (Peloponnes, Griechenland) (1992)
    Berlin : Ges. für Geowiss.
    Associated volumes
    Details Availability
    Call number: SR 90.1144(1)
    In: Schriftenreihe für Geowissenschaften
    Type of Medium: Series available for loan
    Pages: 72 S.
    Series Statement: Schriftenreihe für Geowissenschaften 1
    Language: German
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    BOOK
    Link to Library Catalog
    get availability status
  • 2
    Series available for loan
    Series available for loan
    Rotliegend. Teil 1: Innervariscische Becken; 10. (2012)
    Stuttgart : Schweizerbart
    Associated volumes
    Details Availability
    Call number: S 00.0063(61)
    In: Stratigraphie von Deutschland
    In: Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften
    Type of Medium: Series available for loan
    Pages: 882 S. + 1 Kt.-Beil., graph. darst.
    ISBN: 9783510492251
    Series Statement: Schriftenreihe der Deutschen Gesellschaft für Geowissenschaften 61
    Classification:
    Historical Geology
    Location: Lower compact magazine
    Branch Library: GFZ Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    BOOK
    Link to Library Catalog
    get availability status
  • 3
    Monograph available for loan
    Monograph available for loan
    Jungpleistozäne Strandterrassen in Südost-Lakonien (Peloponnes, Griechenland) (1992)
    Berlin : Verl. der Gesellschaft für geol. Wissenschaft
    Details Availability
    Call number: AWI G1-97-0187
    Type of Medium: Monograph available for loan
    Pages: 72 S. : Ill.
    Series Statement: Schriftenreihe für Geowissenschaften 1
    Branch Library: AWI Library
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    BOOK
    Link to Library Catalog
    get availability status
  • 4
    facet.materialart.
    Unknown
    Outcrops with stratigraphy investigated in Rio Grande do Sul, Brasilia (2016)
    PANGAEA
    In:  Supplement to: Böger, Horst; Kowalczyk, Gotthard (1993): Stratigraphische, sedimentologische und paläoökologische Untersuchungen im Mesozoikum der Depressão Periférica in Rio Grande do Sul, Brasilien. Berichte-Reports, Geologisch-Paläontologisches Institut der Universität Kiel, 63, 72 pp, https://doi.org/10.2312/reports-gpi.1993.63
    Details
    Publication Date: 2024-02-03
    Description: Stratigraphy, sedimentology and paleoecology of Mesozoic continental sequences in the Depressao periferica, Rio Grande do Sui, Brazil, are subject of a DFG (German Research Foundation) research project. Results of the first two years period of activities in which the Geologicai-Paleontological Institutes of the Universities of Kiel and Frankfurt/M. in collaboration with the Departamento de Geociencias, University of Santa Maria in Camobi, RS, were involved are reported here. A second phase of field activities is planned for the time period from fall 1993 to the spring of 1995. The stratigraphic boundaries of the investigation are the underlying sediments of the Permian Passa Dais-Series and the overlying basalts of the Serra Geral Formation, covering the time span of 235 Ma to 133 Ma. A subordinate, chronostratigraphic system encompassing the sediments of this time period has yet to be established and extensive hiatuses are to be expected. Correlations with the lschigualasto Formation in NW-Argentina support the assumption that the upper Santa Maria Formation (Aiemoa member) falls in the mid Carnian. This is the only reasonable certain chronostratigraphic date from the Mesozoic of the Depressao periferica established at the present time. The classical tetrapod sites of the Triassic Santa Maria Formation all fall within the Alemoa-Member, the sediments of which were deposited under in part evaporitic conditions on playa mud flats. Evidence points to isochronic sedimentation and discounts the possibility of a diachronic genesis. The Santa Maria Formation and the underlying Sanga do Cabral Formation are placed together in the Rio do Rasta Subgroup as a genetic unit in accordance with the original definition, which conflicts with present day usage of the names. The Rio do Rasto Subgroup pinches out west of Sao Francisco do Assis and east of the Taquarl river. The entire Rio do Rasto Formation is enclosed in eolic sediments, indicating an extensive sedimentation complex arising from a persistently subsiding playa areal within the Botucatu desert. Beyond the range of the Rio do Rasto Subgroup, it is difficult or impossible to distinguish between the eolic sediments of the older, underlying Rosario do Sui Formation and the overlying, younger Botucatu Sandstone Member. As such, the entire paleogeographically and genetically uniform sedimentation complex is compiled together under the term Botucatu Group. The Sanga do Cabral Formation is characterized by an abundance of detritic micas (muscovite and biotite). K/ Ar dating have indicated a preliminary age for muscovite of 418 ± 8 Ma and 423.5 ± 9.7 Ma. Presumably, they originated from volcanites, subvolcanites and pyroclastics of the Camaqua Group (Brasiliano molasse). As such, the Precambrian/ lower Paleozoic Escudo Sui in Rio Grande do Sui was exposed and eroded to the level found today at the time of deposition of the Sanga do Cabral Formation.
    Keywords: Area/locality; GIK/IfG; Institute for Geosciences, Christian Albrechts University, Kiel; LATITUDE; LONGITUDE; Outcrop; Stratigraphy
    Type: Dataset
    Format: text/tab-separated-values, 841 data points
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    DATA PANGAEA
  • 5
    facet.materialart.
    Unknown
    Kryoturbationsartige Sedimentstrukturen im Pliozän und Altquartär der südlichen Niederrheinischen Bucht: Ein Beitrag zur Unterscheidung kryogener und nichtkryogener Sedimentstrukturen (2011)
    Geozon Science Media
    Details
    Publication Date: 2021-03-29
    Description: Aus fluviatilen Ablagerungen des Jungpliozäns und Altquartärs der südlichen Niederrheinischen Bucht werden Sedimentstrukturen beschrieben, deren Deutung als Kryoturbationen oder Bildungen, die nicht klimabedingt sind, unsicher ist. Genese und Unterscheidungsmöglichkeiten beider Formen werden diskutiert.
    Description: research
    Keywords: 551.7 ; VAR 000 ; Glazialgeologie ; pliozän ; niederrheinische bucht ; altquartär ; kryoturbation ; genese ; sedimentstruktur ; bildungshypothesen ; schichtverfältelung ; bildungsbedingungen ; schichtdeformation
    Language: German
    Type: article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    CITATION GEO-LEO
  • 6
    facet.materialart.
    Unknown
    Tetrapodenfährten aus dem Rotliegenden der Wetterau und ihre stratigraphische Auswertung (1983)
    Details
    Publication Date: 2024-05-28
    Description: Aus den Bleichenbach-Schichten der Wetterau werden folgende Fährtentaxa beschrieben und abgebildet: Saurichnites salamandroides Geinitz, 1861, Saurichnites intermedius Fritsch, 1895, Saurichnites incurvatus Fritsch, 1901, Temnospondylen-Fährte unsicherer systematischer Stellung, cf. Hyloidichnus major (Heyler & Lessertisseur, 1963), Amphisauroides discessus Haubold, 1970, Varanopus microdactylus (Pabst, 1896), Ichniotherium cottae (Pohlig, 1885), Dimetropus leisnerianus (Geinitz, 1863), Gilmo- reichnus kablikae (Geinitz & Deichmüller, 1882), cf. Gilmoreichnus minimus Haubold, 1973, Protritonichnites lacertoides (Geinitz, 1861), Anhomoiichnium orobicum Dozy, 1935, Palmichnus renisus Schmidt, 1959, Laoporus sp. und Jacobiichnus caudifer (Fritsch, 1895). Die Fährtengemeinschaft erlaubt eine Parallelisierung der Bleichenbach-Schichten mit dem oberen Teil der Nahe-Gruppe des Saar-Nahe-Gebietes.
    Description: Abstract: From the Bleichenbach beds of the Wetterau area (lower Permian, SW-Germany) the following ichnotaxa are described and figured: Saurichnites salamandroides Geinitz, 1861, Saurichnites intermedius Fritsch, 1895, Saurichnites incurvatus Fritsch, 1901, temnospondyl-trackway of uncertain systematic range, cf . Hyloidichnus major (Heyler & Lessertisseur, 1963), Amphisauroides discessus Haubold, 1970, Varanopus microdactylus (Pabst, 1896), Ichniotherium cottae (Pohlig, 1885), Dimetropus leisnerianus (Geinitz, 1863), Gilmoreichnus kablikae (Geinitz & Deichmüller, 1882), cf. Gilmoreichnus minimus Haubold, 1973, Protritonichnites lacertoides (Geinitz, 1861), Anhomoiichnium orobicum Dozy, 1935, Palmichnus renisus Schmidt, 1959, Laoporus sp. and Jacobiichnus caudifer (Fritsch, 1895). This trackway-assemblage permits a correlation of the Bleichenbach beds with the upper part of the Nahe Group of the Saar-Nahe Basin.
    Description: 1. Einleitung 2. Vorkommen 3. Terminologie 4. Kurzbeschreibung der Fährten 4.1. Amphibien-Fährten 4.1.1. Saurichnites salamandroides Geinitz, 1861 4.1.2. Saurichnites intermedius Fritsch, 1895 4.1.3. Saurichnites incurvatus Fritsch, 1901 4.1.4. Temnospondylen- Fährte unsicherer systematischer Stellung 4.2. Reptil-Fährten 4.2.1. cf. Hyloidichnus major (Heyler & Lessertisseur, 1963) 4.2.2. Amphisauroides discessus Haubold, 1970 4.2.3. Varanopus microdactylus (Pabst, 1896) 4.2.4. Ichniotherium cottae (Pohlig, 1885) 4.2.5. Dimetropus leisnerianus (Geinitz, 1863) 4.2.6. Gilmoreichnus kablikae (Geinitz & Deichmüller, 1882) 4.2.7. cf. Gilmoreichnus minimus Haubold, 1973 142 4.2.8. Protritonichnites lacertoides (Geinitz, 1861) 4.2.9. Anhomoiichnium orobicum Dozy, 1935 4.2.10. Palmichnus renisus Schmidt, 1959 4.2.11. Laoporussp 4.2.12. Jacobiichnus caudifer (Fritsch, 1895) 5. Fossilinhalt der einzelnen Fundhorizonte 6. Biostratigraphische Auswertung der Fährten 7. Zusammenfassung und Diskussion der Ergebnisse Schriften
    Description: research
    Keywords: ddc:560 ; Hessen ; Rotliegend ; Fährten ; Tetrapoden
    Language: German
    Type: doc-type:article , publishedVersion
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    CITATION GEO-LEO
  • 7
    Electronic Resource
    Electronic Resource
    Die Herkunft der „Porphyr“-Gerölle im Rotliegenden Süd-Hessens (1979)
    Springer
    International journal of earth sciences 68 (1979), S. 805-824 
    Details
    ISSN: 1437-3262
    Source: Springer Online Journal Archives 1860-2000
    Topics: Geosciences
    Description / Table of Contents: Abstract Petrographical and geochemical investigations were carried out to determine the source areas of volcanite pebbles in the Lower Permian Hessischer Trog (southern Chattia, West-Germany). The pebbles of rhyolites have been derived from the Permian rhyolites of the Odenwald-Spessart-Rhön-Uplift in the south. They are restricted to marginal deposits, which accompanied the uplift in a narrow zone. In the corresponding Wetterau-Basin only pebbles of keratophyres have been found, which originated in the Taunus-Uplift in the north. The distribution of pebbles of rhyolites and keratophyres in the Lower Permian conglomerates points out the dominance of the Taunus-Uplift during the Lower Permian. The Taunus-Uplift probably had been devided by a N/S-directed depression which traced out the later Hessische Senke. At the very beginning of the Lower Permian (Unter-Rotliegendes) a barrier had existed in front of the Spessart-Uplift — probably composed of the “Nordliche Gneise” — which became an area of deposition later on in the Lower Permian.
    Abstract: Résumé Cette étude a pour but de rechercher la source des cailloux volcaniques du Permien inférieur du bassin méridional d'Hesse à l'aide des méthodes pétrographiques et géochimiques. Les cailloux rhyolithiques, dérivés du haut-fond Odenwald-Spessart-Rhön se rencontrent seulement dans les sédiments d'une zone étroite au bord de ce haut-fond. Dans le bassin de la Wetterau les conglomérats contiennent prèsque exclusivement des cailloux keratophyriques qui proviennent de la partie septentrionale du haut-fond du Taunus. La distribution des cailloux rhyolithiques et keratophyriques démontre que toujours le haut-fond du Taunus a été plus important que le seuil du Spessart. En outre il est probable que le haut-fond du Taunus a été subdivisé par une dépression transversale de direction N-S qui indique déjà la future Hessische Senke. Au début du Rotliegend inférieur une barrière a existé devant le seuil du Spessart qui avait été compris dans la région de la sédimentation au cours du Rotliegend.
    Notes: Zusammenfassung Mit Hilfe petrographischer und geochemischer Untersuchungsmethoden wurde versucht, die Liefergebiete der Gerölle saurer Vulkanite im Unter-Perm des sdlichen Hessischen Troges zu ermitteln. Dabei zeigte sich, daß Rhyolith-Gerölle, angeliefert von den Rhyolithvorkommen der Odenwald-Spessart-Rhön-Schwelle, nur auf das schmale Gebiet der Schwellenrand-Sedimente beschränkt sind. Im eigentlichen Becken der Wetterau führen die Konglomerate nahezu ausschließlich Keratophyr-Gerölle, die von der nördlich gelegenen Taunus-Schwelle stammen. Die Verteilung der Rhyolith- und Keratophyr-Gerölle in den Rotliegend-Konglomeraten deutet auf eine stete Dominanz der Taunus-Schwelle gegenüber der Spessart-Schwelle. Es läßt sich ferner wahrscheinlich machen, daß die Taunus-Schwelle durch eine N-S-streichende Querdepression gegliedert war, die die spätere Hessische Senke bereits vorzeichnet. Der Spessart-Schwelle war im basalen Unter-Rotliegenden eine Barriere nördlich vorgelagert („Nördliche Gneise“), die im Laufe des Rotliegenden in den Ablagerungsraum einbezogen wurde.
    Type of Medium: Electronic Resource
    URL: http://dx.doi.org/10.1007/BF01820819
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    Paper (German National Licenses)
    Fulltext
  • 8
    facet.materialart.
    Unknown
    A Synoptic View on the Neotectonic Development of the Peloponnesian Coastal Regions (1976)
    Schweizerbart
    Details
    Publication Date: 1976-01-01
    Print ISSN: 0012-0189
    Topics: Geosciences
    Published by Schweizerbart
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    PAPER CURRENT
  • 9
    facet.materialart.
    Unknown
    The Geological Development of the Kyllini Peninsula (Western Peloponnesos, Greece) during Neogene ans Quaternary (1979)
    Schweizerbart
    Details
    Publication Date: 1979-01-10
    Print ISSN: 0012-0189
    Topics: Geosciences
    Published by Schweizerbart
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    PAPER CURRENT
  • 10
    facet.materialart.
    Unknown
    Occurrences of the Olonos-Pindos Series in SE Laconia (Peloponnesos) (1986)
    Schweizerbart
    Details
    Publication Date: 1986-01-01
    Print ISSN: 0012-0189
    Topics: Geosciences
    Published by Schweizerbart
    Location Call Number Expected Availability
    BibTip Others were also interested in ...
    PAPER CURRENT
Close ⊗
This website uses cookies and the analysis tool Matomo. More information can be found here...