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  • 1
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    Ein neuer Eryopoide (Amphibia: Temnospondyli) aus dem saarpfälzischen Rotliegend (Unter-Perm; Südwest-Deutschland) (1996)
    Details
    Publication Date: 2022-09-14
    Description: Palatinerpeton kraetschmeri n. gen. n. sp. aus dem unteren Rotliegend (äquivalent Asselium) des Saar-Nahe-Beckens wird an Hand des Holotypus beschrieben. Überliefert sind Partien des ventralen Schädeldaches, des Gaumens und des Postkranialskelettes sowie der komplette Unterkiefer. Aus einem vorläufigen Cladogram der Edopoidea und Eryopoidea ergibt sich: Palatinerpeton repräsentiert eine plesiomorphe Entwicklungslinie innerhalb der Eryopoidea, die sich keiner bekannten Familie zuordnen läßt. Im Schädel weist er wenige, auffällige Übereinstimmungen mit fortschrittlicheren, stratigraphisch jüngeren Taxa auf; so mit Lysipterygium (Jugalfortsatz am Vorderrand des Postorbitale), den Melosauridae (Alar-Fortsatz des Jugale) sowie einem Melosauriden und den Cochleosauridae (Trennung Maxillare-Quadratojugale durch Zwischenschaltung des Jugale).
    Description: Abstract: Palatinerpeton kraetschmeri n. gen., n. sp., from the lower Rotliegend (Lower Permian: Asselian equivalent) of the Saar-Nahe Basin is described on the basis of the holotype. The holotype preserves portions of the skull roof in ventral view, parts of the palate and postcranial skeleton, and the complete lower jaw. A preliminary phylogenetic analysis of the Edopoidea and Eryopoidea suggests that Palatinerpeton represents a plesiomorphic taxon among the Eryopoidea and cannot be referred to any known family. The skull of Palatinerpeton shares a few noteworthy resemblances with more derived, stratigraphically more recent taxa: It shares with Lysipterygium the presence of a jugal process on the anterior margin of the postorbital, with the Melosauridae the presence of an alary process of the jugal, and with one melosaurid and the Cochleosauridae the separation of the maxilla and quadratojugal by the jugal.
    Description: research
    Keywords: ddc:567
    Language: German
    Type: doc-type:article , publishedVersion
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  • 2
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    Palynofacies studies of lake sediments with examples from the Saar-Nahe Basin (Permocarboniferous; SW-Germany) (1996)
    Details
    Publication Date: 2022-10-17
    Description: Abstract: A provisional palynological organic matter classification is applied for the palynofacies from lacustrine sediments of the uppermost Carboniferous and lowermost Permian of Southwest-Germany (Rotliegend). Sedimentary organic matter of mainly higher biological origin is determined microscopically. The definition of three fixed major- and variable subdivisions led to the creation of seven palynofacies types. These PF-Types are in addition graphically defined by a ternary diagram, a palynofacies-triangle. 30 lake horizons of different stratigraphic positions and their surrounding environments were studied and the results compared to each other. A preliminary model provides an overview on relations between PF-Types and corresponding environments. Differences in the palynofacies composition of the pelagial facies help to characterise the relative size of fossil lakes. The results from the sedimentary sequences of whole lake successions in comparison are partially blurred and have to be analysed separately. In these successions the complete development of one lake is documented by the palynofacies. The PF-analyses provide valuable data and lead to more accurate reconstructions of fossil lake environments, especially its inhabitants.
    Description: Kurzfassung: Eine vorläufige Klassifikation für palynologische organische Materie wird auf die Palynofazies lakustriner Sedimente des obersten Karbon und unteren Perm (Rotliegend) Südwestdeutschlands angewandt. Das sedimentäre organische Material mit weitgehend höherer biologischer Herkunft wurde mikroskopisch bestimmt. Die Definition dreier festgelegter Haupt- und variabler Unterabteilungen führte zur Bildung von sieben Palynofazies-Iypen. Diese PF-Typen werden zusätzlich graphisch durch ein ternäres Diagramm, ein „Palynofazies-Dreieck”, definiert. Dreißig Seehorizonte unterschiedlicher stratigraphischer Position und ihre umgebende Umwelt wurden untersucht und die Ergebnisse miteinander verglichen. Ein vorläufiges Modell bietet einen UÜberblick über Beziehungen zwischen PF-Typen und korrespondierendem Environment. Unterschiede in der Zusammensetzung der Palynofazies helfen die relative Seegröße zu bestimmen. Ergebnisse von den vollständigen sedimentären Abfolgen sind vergleichsweise partiell undeutlich und müssen getrennt analysiert werden. In diesen Abfolgen wird die komplette Entwicklung eines Sees durch seine Palynofazies dokumentiert. Die PF-Analyse liefert somit wertvolle Daten und führt zu genaueren Rekonstruktionen fossiler Lebensräume im See, speziell seiner Bewohner.
    Description: research
    Keywords: ddc:551.304
    Language: English
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  • 3
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    Aufbau, Alter und regionale Einordnung der Endmoränen im Gebiet des Falken-Berges bei Fallingbostel (Niedersachsen) . (1983)
    Geozon Science Media
    Details
    Publication Date: 2022-08-04
    Description: In dem Hügelgebiet um den Falken-Berg zwischen Fallingbostel und Bergen Kr. Celle zeichnen sich 3 Endmoränenbögen ab, der Örbker, der Becklinger und der wenig deutlich ausgeprägte Kl. Bockeler Endmoränenbögen. Örbker und Kl. Bockeler Endmoränenbögen verdanken ihre Entstehung Gletscherloben, die von NW heranrückten; der Becklinger Endmoränenbögen geht auf einen von NE heranrückenden Lobus zurück. Keine dieser Endmoränen ist vom nordischen Inlandeis überfahren worden. Ein nahe den Endmoränenbögen wurzelnder Fächer aus Schmelzwasser-Ablagerungen läßt sich bis nahe an die Aller-Niederung heran verfolgen. Er überlagert die drenthestadiale Hauptmoräne, ist also jünger als diese. Die Endmoränen zwischen Fallingbostel und Bergen sind in einer späten Phase des Drenthe-Stadiums der Saale-Eiszeit entstanden.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 4
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    Th-230 / U-234- sowie ERS-Altersbestimmungen einiger Travertine in Ungarn (1983)
    Geozon Science Media
    Details
    Publication Date: 2022-08-05
    Description: Dreizehn Travertinproben von den Lokalitäten Tata, Vértesszöllös, Dunaalmás und Buda werden mit Hilfe zweier neuerer Absolutdatierungsverfahren untersucht, der Th-230/U-234- und der ESR-Methode. Für acht der untersuchten Proben ergibt sich eine gute Übereinstimmung zwischen den Th/U- und den ESR-Altern, zwei Proben waren aufgrund extrem hoher Mangan-Gehalte nicht ESR-datierbar und in drei Fällen ergaben sich deutliche Diskrepanzen. Travertine aus dem Riß/Würm Interglazial haben ein Alter von ca. 100.000 a, die des vorletzten Interglazial zeigen ein Alter von 200.000 a und etwas darüber die des drittletzten Interglazials weisen ein Alter von über 300.000 a auf.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 5
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    Die geomorphologisch-bodengeographische Deutung der pleistozänen Sedimente und der fossilen Böden an der Playa de Baranán (westl. La Coruna) und bei Cangas de Foz (Nord-Galizien) (1983)
    Geozon Science Media
    Details
    Publication Date: 2022-08-05
    Description: Aus dem nördlichen Galizien (NW-Spanien) werden von zwei Lokalitäten (Playa de Barañán, westl. La Coruña, und Cangas de Foz, westl. Ribadeo) jungpleistozäne Sediment-Boden-Folgen beschrieben, die auf einem 3—5 m ü. M. gelegenen Felssockel bzw. auf einer ca. 25 m ü. M. gelegenen Küstenterrasse auflagern. Mehrere 14C-Daten sowie Vergleiche mit früher aufgenommenen Sediment-Boden-Folgen in der näheren und weiteren Umgebung lassen den Schluß zu, daß in beiden Fällen eine nahezu vollständige würmzeitliche Schichtenfolge entwickelt ist, die von fossilen Braunerden bzw. kräftigen fossilen Ah-Horizonten gegliedert ist. Zwischen die fossilen Böden bzw. Bodensedimente sind möglicherweise äolisch entstandene Schlurfe bzw. Sande und Solifluktionsschuttdecken eingeschaltet. Die wahrscheinlich altwürmzeitlichen Profilteile zeichnen sich durch viel Holzkohle aus und weisen auf eine holzreiche Vegetation hin.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 6
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    Sedimentologische Zuordnung saalezeitlicher Gletscherablagerungen zu mehreren Vorstößen am unteren Niederrhein (1983)
    Geozon Science Media
    Details
    Publication Date: 2022-08-05
    Description: Beim Vorstoß sowie Rückzug des Eises werden Sandersedimente abgelagert. Sie setzen sich aus gröberen Vorschütt- und feineren Nachschüttsanden zusammen, die (meistens) durch eine Grundmoräne voneinander getrennt sind. Vorschüttsand, Grundmoräne und Nachschüttsand bilden einen glaziären Zyklus. Fehlt die Grundmoräne, so ist eine genetische Gliederung der Sedimente in eine Vorstoß- und Rückzugsphase erschwert. Bei der Sedimentuntersuchung zeigte sich, daß einzelne Korngrößenfraktionen für eine Gliederung des Sanders kaum von Bedeutung sind. Die Zusammenfassung von Korngrößenfraktionen zu Korngrößengruppen (Tab. 1) ermöglichte eine exakte Gliederung der Sandersedimente und damit die genetische Ansprache der Gletscherablagerungen am unteren Niederrhein. Aufgrund der Einlagerung von Grundmoränenmaterial in den Sandersedimenten konnten für das Drenthe-Stadial im Raum Louisendorf-Moyland drei Eisvorstöße nachgewiesen werden.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 7
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    „Orbulina” bituminosa SPANDEL, 1909, ein Mikroproblematikum aus dem Fischschiefer (Rupelium) des Mainzer Beckens (1996)
    Details
    Publication Date: 2022-09-20
    Description: Im Fischschiefer (Rupelium) des Mainzer Beckens werden häufig hohle Kugeln von etwa 200 m Durchmesser gefunden. SPANDEL (1909) hat diese als Orbulina bituminosa beschrieben und den Foraminiferen zugeordnet. Aufgrund der Ähnlichkeiten von Größe und Struktur werden die Kugeln als Crustaceeneier interpretiert.
    Description: Abstract: Hollow - 200 pım diameter spheres have been frequently found in the Rupelian „Fischschiefer” of the Mainz Basin. SPANDEL (1909) first described them as Orbulina bituminosa and interpreted them as foraminifera. The prefered interpretation of the spheres is that they are Crustacean eggs because of similarities both in terms of size and internal structure.
    Description: research
    Keywords: ddc:562
    Language: German
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  • 8
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    Rotliegend-Ignimbrite in der Prims-Mulde (Saar-Nahe-Senke/Südwestdeutschland) (1983)
    Details
    Publication Date: 2022-12-22
    Description: Die oberrotliegenden rhyolithischen Tuffe der Prims-Mulde werden als Ignimbrite interpretiert. Sie sind maximal 110 m mächtig, gliedern sich durch wenige air-fall-Tuffe in mehrere Einheiten und können auf beiden Flanken der Prims-Mulde bis zu ca. 13 km weit verfolgt werden. Abgeplattete Bimse, Phänokristalle und zahlreiche Xenolithe treten in einer rötlichen, gering verschweißten Matrix auf. Die nicht dem Rotliegenden entstammenden Xenolithe, ihre Verteilung und die Ausrichtung von Bimslängsachsen weisen auf ein Liefergebiet für die pyroklastischen Ströme im Hunsrück hin. Gleichartig ausgebildete pyroklastische Ströme treten im Rotliegenden des Wittlicher Troges auf. Beide Vorkommen werden auf den im Hunsrück gelegenen, in devonische Gesteine eingebetteten Veldenzer Rhyolithschlot bezogen, der eine initiale Ignimbrit- Phase aufwies und wahrscheinlich den Förderort für die Vorkommen in den beiden Rotliegendtrögen darstellt.
    Description: Abstract: Rhyolithic tuffs within the Prims syncline of the Permocarboniferous late Hercynian intermontane Saar-Nahe trough, SW Germany, are interpreted as pyroclastic flow deposits. They are highly altered, weakly welded, and separated by thin air-fall tuffs. Their regional extent, petrography and xenolith content is described. The Devonian provenance of the xenoliths, their distribution, and the Orientation of the flattened pumice fragments all point to the Hunsrück north of the Saar-Nahe trough as the area the pyroclastic flows came from. The pyroclastic flows and similar flows in the next trough to the northwest, the Wittlich trough, are related to the Veldenz rhyolite in the Hunsrück which contains an initial ignimbrite phase and is considered to represent the feeder for these pyroclastic flows.
    Description: 1. Einleitung 2. Geologische Situation 3. Die Ignimbritfolge 3.1. Verbreitung, Volumen, Paläogeographie 3.2. Ausbildung der Ignimbrite 3.3. Abfolge der Ignimbrite 3.4. Beschreibung der Profile 3.5. Petrographie und Chemie 3.5.1. Ignimbrit-Typ Eisen 3.5.2. Ignimbrit-Typ Lauxwald 4. Die Xenolithe der Ignimbritfolge 4.1. Grünliche, grobkörnige Sandsteine 4.2. Feinsandsteine, Silt- und Tonsteine 4.3. Quarzite 4.4. Phyllite . 4.5. Chloritschiefer 5. Gesteine aus dem Rotliegenden und Unterdevon 6. Die Herkunft der Ignimbrite Schriften
    Description: research
    Keywords: ddc:554.3 ; Saar-Nahe-Becken ; Rotliegend ; Ignimbrite
    Language: German
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  • 9
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    Tetrapodenfährten aus dem saarpfälzischen Rotliegenden (? Ober-Karbon - Unter-Perm; Südwest-Deutschland) (1983)
    Details
    Publication Date: 2023-12-05
    Description: Es werden Morphologie, Proportionen und Belastungsverhältnisse der Fährtentaxa Saurichnites salamandroides Geinitz, 1861, Saurichnites incurvatus Fritsch, 1901, Saurichnites intermedius Fritsch, 1895, Limnopus palatinus nov. ichnospec., Amphisauroides sp., Protritonichnites lacertoides (Geinitz, 1861), Gilmoreichnus kablikae (Geinitz & Deichmüller, 1882), Gilmoreichnus minimus Haubold, 1973, Hyloidichnus arnhardti Haubold, 1973 und Jacobiichnus caudifer (Fritsch, 1895) beschrieben. Außerdem werden die Körperproportionen der fährtenerzeugenden Tiere in hypothetischer Form rekonstruiert und ihre orthotaxonomische Position diskutiert.
    Description: Abstract: Morphology, proportions and pressure distribution of the ichnotaxa Saurichnites salamandroides Geinitz, 1861, Saurichnites incurvatus Fritsch, 1901, Saurichnites intermedius Fritsch, 1895, Limnopus palatinus nov. ichnospec., Amphisauroides sp., Protritonichnites lacertoides (Geinitz, 1861), Gilmoreichnus kablikae (Geinitz & Deichmüller, 1882), Gilmoreichnus minimus Haubold, 1973, Hyloidichnus arnhardti Haubold, 1973 and Jacobiichnus caudifer (Fritsch, 1895) are described. In addition to this the body-proportions of the trackway-producing animals are reconstructed hypothetically. The orthotaxonomic position of these animals is discussed.
    Description: 1. Einleitung 2. Fundorte und Fundschichten 3. Terminologie der Fährten. 4. Beschreibung der Fährten 4.1. Saurichnites salamandroides Gbinitz, 1861 4.2. Saurichnites incurvatus Fritsch, 1901 4.3. Saurichnites intermedius Fritsch, 1895 4.4. Limnopus palatinus nov. ichnospec. 4.5. Amphisauroides sp. 4.6. Protritonichnites lacertoides (Geinitz, 1861) 4.7. Gilmoreichnus kablikae (Geinitz & Deichmüller, 1882) 4.8. Gilmoreichnus minimus Haubö'lt), 1973 4.9. Hyloidichnus arnhardti Haubold, 1973 4.10. Jacobiichnus caudifer (Fritsch, 1895) 5. Schlußbemerkungen Schriften
    Description: research
    Keywords: ddc:562 ; Saar-Nahe-Becken ; Tetrapoden ; Rotliegend
    Language: German
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  • 10
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    Neue Forschungsmöglichkeiten in der Paläontologie an unterdevonischen Brachiopoden (Emsium) aus dem südlichen Rheinischen Schiefergebirge (1996)
    Details
    Publication Date: 2023-03-10
    Description: Ein Vergleich von neueren Publikationen über die intraspezifische Variabilität bei rezenten Brachiopoden und die Genese von Schilien mit älteren publizierten Daten über unterdevonische (Emsium, ohne Hunsrückschiefer) Brachiopoden erlaubt mit Hilfe von Überlegungen zur Funktions- und Konstruktionsmorphologie die Formulierung von neuen Forschungsperspektiven. Sie betreffen die Bereiche: Taxonomie, Phylogenese, Biostratigraphie und Paläoökologie der unterdevonischen Brachiopoden.
    Description: Abstract: Recent literature on the intraspecific variability of recent brachiopods, the genesis of shell beds and considerations concerning functional and constructional morphology compared with so far published data on Lower Devonian (Emsium, Southern Rheinisches Schiefergebirge, Hunsrück slate excluded) brachiopods, allow to formulate new perspectives of research. They concern the disciplines: Taxonomy, phylogeny, biostratigraphy and paleoecology of the Lower Devonian brachiopods.
    Description: research
    Keywords: ddc:562 ; Brachiopoden ; Unterdevon ; Rheinisches Schiefergebirge
    Language: German
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  • 11
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    Probleme bei der modernen landwirtschaftlichen Moornutzung (1983)
    In:  SUB Göttingen | ZA 34278
    Details
    Publication Date: 2024-02-28
    Description: Nahezu zwei Drittel aller Hochmoore und fast alle Niedermoore werden in Niedersachsen landwirtschaftlich − überwiegend als Grünland − genutzt. Aktuelle Nutzungsprobleme liegen z.Zt. innerbetrieblich im Bereich der Erhaltung der Bodenfruchtbarkeit bei Anpassung an die gesamtwirtschaftliche Entwicklung. Kleine moorreiche Betriebe unterliegen dem Zwang zu höchster Flächenproduktivität. Mit Überschreiten einer Düngungsintensität von 200 kg/ha N und 80 kg/ha P2O5 entstehen hohe Gewässerbelastungen und verstärkter Torfschwund. Eine mehr konservierende Bodennutzung, z.B. durch Sanddeckkulturen wird empfohlen, anderenfalls sind die ökologisch tolerierbaren Grenzen der Intensivierung auf Moorschwarzkultur bald überschritten. Größere Betriebe mit geringeren Mooranteilen versuchen mit dem Ziel einer besseren Arbeitsproduktivität diese durch Tiefumbruch in ihr Mineralbodennutzungskonzept zu integrieren. Nur extensiv genutztes Moorgrünland genügt den Ansprüchen von Naturschutz und Landespflege. Entsprechende Zugeständnisse der Landwirtschaft im Nahbereich von Naturschutzgebieten machen als Ausgleich intensivere Nutzungen auf den übrigen Flächen erforderlich. Einer Zwischenabtorfung von Hochmoorkulturen kann landeskulturell nur zugestimmt werden, wenn die landwirtschaftliche Folgenutzung über eine Sandmischkultur zu einer wirklichen Standortsverbesserung führt.
    Description: About two third of the raised bog areas and nearly 100% of the fen areas in Lower Saxony are agriculturally used, mainly as grassland. Today actual problems in agricultural utilization of peatlands are internal problems of the farms in respect to the preservation of soil fertility along with the adaption to the general economical development. Small farms, rich in peatland, are forced to highest land productivity. However, a fertilizing intensity of more than 200 kg/ha nitrogen and 80 kg/ha phosphorus causes water contaminations and peat losses. A more conservative utilization of peatlands, e.g. by sand-cover cultivation, is therefore recommended. Otherwise an intensification of raised bog and fen utilization would soon exceed the ecologically allowable limits. Large farms with small amounts of peatland try to attain a better productivity of work by deep ploughing and integration of sand-mix cultivated peatlands into the conception of utilizing their mineral soils. The claims of nature conservation and landscaping are only satisfied in case of extensively used grassland on peat. Corresponding concessions of farmers to areas close to nature reserves require agreements for a more intensive utilization of other areas. An intermediate peat cutting on formerly cultivated raised bogs should only be allowed if deep ploughing and sand-mix cultivation creates a really improved soil for later agricultural utilization.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:630.914 ; Moor ; Torf ; Landnutzung ; peatland ; peat ; land use
    Language: German
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  • 12
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    Beschaffenheit und hydrogeologische Zusammenhänge des tieferen Grundwassers im nördlichen Stadtgebiet von Berlin (West) (1983)
    Reimer
    In:  Herausgeberexemplar
    Details
    Publication Date: 2024-04-08
    Description: Die Untersuchungen der Grundwasserbeschaffenheit und der hydrogeologischen Zusammenhänge erstrecken sich auf das nördliche Stadtgebiet von Berlin (West), das ein Teil des Einzugsgebietes der oberen Havel ist. Das betrachtete Grundwassersystem erfaßt die im Hangenden des mittel oligozänen Septarientons in normaler stratigraphischer Abfolge ausgebildeten Ablagerungen des Oberoligozäns, Miozäns und Pleistozäns Die Mächtigkeiten der auftretenden Schichtfolgen sind abhängig von einer durch Salzbewegungen verursachten Aufwölbung im NE und einer im W gelegenen Salz-Emigrationszone. Folglich treten die größten Mächtigkeiten (ca. 380 m) im W des Untersuchungsgebietes auf. Die pleistozänen Ablagerungen erreichen ihre größten Mächtigkeiten im Bereich einer Erosionsrinne, die im mittleren Teil des Untersuchungsgebietes bis in den Septarienton eingeschnitten ist. Die Betrachtung der Druck- und Fließverhältnisse zeigt sowohl für das tiefere, gespannte Grundwasser der tertiären Schichtfolgen als auch für den oberen Grundwasserleiter einen hauptsächlich nach SW gerichteten Grundwasserabstrom. Für die Potentialdifferenzen zwischen dem oberen und dem gespannten Grundwasser kann in den Bereichen großer Grundwasserentnahmen ein relatives Ansteigen der Druckfläche des tieferen Grundwassers erkannt werden. Die höhere Druckfläche des tieferen Grundwassers weist, in Abhängigkeit von der Durchlässigkeit der stauenden Schichten, auf ein Aufsteigen tieferer Grundwässer hin. Dies wird bekräftigt durch die Ergebnisse der geothermischen Untersuchungen, die für die entsprechenden Bereiche eine großflächige positive geothermische Anomalie erkennen lassen. Der Chemismus der untersuchten Grundwässer läßt im allgemeinen mit zunehmender Tiefe eine Abnahme der Gesamtmineralisation erkennen. Die durchschnittliche Gesamtmineralisation der tieferen Grundwässer liegt mit 15.07 mval/1 unter der des Grundwassers der pleistozänen Schichten (17.38 mval/1). Die räumliehe Betrachtung der Mineralisationsverteilung läßt für die tieferen Grundwässer im NE- und SE-Teil des Untersuchungsgebietes eine erhöhte Mineralisation erkennen, die hauptsächlich auf höhere Kalziumsulfatgehalte zurückzuführen ist. In westlicher Richtung kommt es, durch Reduktionsvorgänge, zu einer Abnahme der Mineralisation. Im tieferen Bereich der Rinne und in den oberoligozänen Schichtfolgen läßt sich das Auftreten von alkalihydrogenkarbonathaltigen Wässern erkennen, deren Entstehung auf Ionenaustauschvorgänge zurückzuführen ist. Die Spurenmetallgehalte zeigen im Grundwasser der tertiären Schichtfolgen, bedingt durch die auftretenden Gesteine, für die Elemente Aluminium, Kupfer und Zink deutlich höhere mittlere Gehalte. Die gegenüber dem Grundwasser der oberoligozänen Schichtfolgen höheren mittleren Bor-, Kupfer- und Nickelgehalte im Grundwasser der miozänen Schichten stehen in Verbindung mit der primären Anreicherung dieser Elemente in den organischen Ablagerungen des Miozäns. Für das Auftreten der Elemente Chrom (III), Strontium und Eisen lassen sich keine Unterschiede zwischen dem tiefen und dem oberflächennahen Grundwasserleiter erkennen.
    Description: The quality of groundwater and hydrogeological relationships of the northern part of the town of Berlin (West), a catchment area of the upper part of the river Havel, were investigated. The observed groundwater System belongs to the stratas above the middle oligocene "Septarienton", in the normal sequence of upper oligocene, miocene and pleistocene. The thicknesses of the occuring layers are influenced by a salt dorne in the NE and a rim syncline in the W, caused by salt tectonics. Consequently the greatest thickness (~380m) is found in the Western part of the investigated area. The pleistocene deposits obtain their greatest thickness in the area of an erosion channel which is in the middle of the investigated area, incised into the middle oligocene Septarienton. The investigations of the relations between artesian head and groundwater flow of the deeper confi ned groundwater in the tertiary strata and of the upper aquifer proved a groundwater flow mainly in southwestern direction. The potential differences between the upper and the confined groundwater shows in the areas of ground-water lowering a relative rising of the hydrostatic pressure of the deeper groundwater. The higher artesian head of the deeper groundwater points to a rise of deeper groundwater, dependent on the permeability of the less permeable layers. This is confi rmed by the results of the geothermical investigations, which show a great positiv geothermal anomal y for these areas. The Chemical composition of the investigated groundwater shows a decreasing total mineral isation with increasing depth. The average total -mineral isation of the deeper groundwater of 15.07 mval/1 lies beneath the level of the groundwater of pleistocene layers (17.38 mval/1). Spacial observations of the mineral isation-distribution show a higher mineral isation for the deeper groundwater in the NE- and SE-part of the investigated area, which is mainly based on a higher calcium-sulfat-content. In the W a decrease of mineral isation, caused by reduction processes, can be observed. In the deeper part of the channel and in the upper oligocene layers an occurrence of alkali-hydrogencarbonat-water, caused by ion-exchange reactions, is recognizable. Trace-metalls contents in the groundwater of the tertiary layers have a definite higher average content of the elements Al, Cu and Zn, caused by the occuring Sediments. The concentration of B, Cu and Ni is higher in the groundwater of the miocene layers than in the groundwater of the upper oligocene layers, this is caused by the primary enrichment of these elements in the organic deposits of the miocene. There are no differences recognicable between the upper and the lower aquifers concerning the occurrence of the elements Co(III), Sr and Fe.
    Description: Les recherches concernant la composition de l'eau souterraine et les relations hydro-geologiques Interessent la partie nord de la ville de Berlin (Ouest), qui fait partie de l'aire d'al imentation de la Havel superieure. Le Systeme de l'eau souterraine considere englobe les Sediments de l'oligocene superieur, du miocene et du pleistocene, surmontant strati graphiquement les couches de l'oligocene moyen (Septarienton). Les puissances des differentes series strati graphiques sont influencees par un bombement au Nord-Est, du ä une tectonique salifere, et par une zone d'emigration salifere situee a' l’ouest. En consfequence les puissances maximales (environ 380m) apparaissent dans la partie ouest du terrain analyse. Les formations du pleistocene atteignent leur plus grande epaisseur au niveau d'une gouttiere d'erosion pentue, encaissee dans la partie moyenne du terrain analyse jusqu'au Septarienton. L'observation des conditions de pression et d'ecoulement montre, tant pour l'eau souterraine profonde et captive des suites de couches tertiaires, tant pour les aquiferes superieurs, un ecoulement principalement vers le Sud-Ouest. Pour les differences de pression entre les eaux souterraines superieures et captives on note dans les terrains, desquels on preleve beaucoup d'eau, un soulevement relatif de la surface de pression de l'eau souterraine profonde. Le plus haut plan de pression de celle-ci indique donc que les eaux souterraines profondes montent en fonction de la permeabilite des couches accumulees. Ceci est renforce par les resultats des analyses geothermiques, qui montrent une anomal ie geothermique positive sur une grande surface des terrains en question. Les caracteri stiques hydrogeochimiques des eaux souterraines analysees font apparaTtre en general une diminution de la mineral isation totale en fonction de 1 ’augmentation de la profondeur. La mineral isation totale moyenne des eaux profondes souterraines est avec 15.07 mval/1 inferieure ä celle des eaux profondes des couches pleistocenes(17. 38 mval/1). La repartition horizontale de la mineral isation laisse apparaTtre pour les eaux profondes de la partie Nord-Est et Sud-Est du terrain analyse une mineral isation surelevee, qui est due principalement a une haute teneur en Sulfate de calcium. Vers 1 'ouest, la mineral isation diminue par l'effet de processus de rfeduction. Dans les terrains du fond de la gouttiere et dans les series de couches de l'oligocene superieur on remarque l'apparition d'eaux contenant du NaHCOp provenant du processus de changements des ions. Les teneurs de metaux traces dans les eaux souterraines des series tertiaires montrent nettement-conditionne par les roches y apparaissant- des valeurs moyennes elevees pour l’aluminium, le cuivre et le zinc. Les teneurs moyennes en bore, cuivre et nickel des eaux souterraines des couches du miocene, surelevees par rapport aux eaux souterraines des couches de l'oligocene superieur, sont en relation avec l'enrichissement primaire de ces elements dans les gisements organiques du miocene. En ce qui concerne la repartition des eie ments chrome( III), Strontium et fer aucune difference est notable entre les aquiferes profonds et ceux pres de la surface.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.79 ; Grundwasser
    Language: German
    Type: doc-type:book
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  • 13
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    Unknown
    Entwicklung einer oberjurassischen Karbonatplattform (1996)
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Details
    Publication Date: 2024-04-17
    Description: In der Zentralen Dobrogea in Ostrumänien liegen die östlichsten europäischen Vorkommen oberjurassischer Mikrobialith/Kieselschwamm-Gesteine (Spongiolithe). Im Oxfordium existierte in der Zentralen Dobrogea eine flach nach Westen geneigte Karbonatplattform (homoklinale Rampe), auf der verschiedene kieselschwamm- und korallendominierte Rifftypen auftraten. Die Entwicklung der Karbonatrampe begann mit einer raschen Transgression im unteren Oxfordium. Gegen Ende der transgressiven Phase konnten sich in Wassertiefen unterhalb ca. 25 m Schwammrasen etablieren, in der Hochstandsphase schließlich auch Kieselschwamm/Mikrobialith-Bioherme. Ein für die rumänischen Vorkommen charakteristischer ringförmiger Biohermtyp spiegelt vermutlich ein präexistierendes Relief des Untergrundes wieder. Diese Kieselschwamm/Mikrobialith-Riffe besaßen ein früh zementiertes rigides Gerüst aus mikrobiellen Automikriten, das in erster Linie von lithistiden Demospongien und von hexactinelliden Kieselschwämmen besiedelt war. Deren Skelette wurden nach ihrem Absterben ebenfalls mikrobiell zementiert und kalzifiziert. Die Reste ihrer Skelette sind in den Riffen untergeordnet überliefert, in den Biostromen dominieren sie jedoch gegenüber Mikrobialithen. Diese Mikrobialith-Kieselschwamm-Bioherme besiedelten die mittlere Rampe in Wassertiefen, die unterhalb der Schönwetter-Wellenbasis lagen und nur bei schweren Stürmen von der Sturmwellenbasis erreicht wurden. Auf der äußeren Rampe von Sturmwellen nicht erreichbar entwickelten sich gleichzeitig kleine Thrombolith-Kieselschwamm-Mudmounds, an denen vorwiegend Hexactinellida beteiligt waren. Landwärts verzahnten sich die Spongiolithe mit kalkigen Areniten. In Wassertiefen vermutlich um 10 bis 15 m traten die ersten sehr dünnplattigen hermatypen Korallen auf und bildeten weite Biostrome (Fungiiden-Biostrome). Gründe für die Ablösung der Mikrobialith-Kieselschwamm-Assoziation durch hermatype Korallen erst in so flachem Wasser sind zum einen die geringe Toleranz der Mikrobialith-Kieselschwamm-Assoziation gegenüber stärkerer Wasserbewegung mit erhöhten Sedimentations- und Sedimentumlagerungs-Raten. Zum anderen hinderte möglicherweise eine Einschränkung der euphotischen Zone durch ein zeitweise leicht erhöhtes Nährstoffangebot mit Planktonblüte und dadurch verringerter Wassertransparenz hermatype Korallen daran, in tiefere Bereiche vorzudringen. Die im oberen Oxfordium einsetzende Regression führte zur Progradation der lagunären und bioklastischen Fazies der inneren Rampe. In dieser retrograden Phase entstanden Korallen-Fleckenriffe im hochenergetischen Flachwasser und Korallen-Stromatoporen-Chaetetiden-Fleckenriffe in den flachsten Teilen der mittleren Rampe. Die Schwamm-Mikrobialith-Assoziation verschwand zuerst in der östlichen Zentralen Dobrogea. In landferner Position im Westteil der Zentralen Dobrogea wurde sie etwas später von Korallenvorkommen abgelöst.
    Description: The Central Dobrogea in Eastern Romania exhibits the easternmost occurrence of Upper Jurassic microbialite/siliceous sponge facies (spongiolite facies) in Europe. The spongiolites are part of the Lower to Upper Oxfordian Casimcea Fm. which was deposited on a gently westward dipping carbonate platform (homoclinal ramp). This platform was surrounded by deep marine basins in the south, west and north, while to the east the existence of a land area with low relief is assumed. The gently sloping carbonate ramp shows an E-W facies zonation. A lagoonal belt is followed towards the open sea by a coral patch reef belt, a bioclastic-oolitic sand belt, and a spongiolitic belt. The lagoonal belt is rich in structureless to laminated microbial crusts, which occasionally exhibit prism cracks and comprise bioclasts and dark lithoclasts ("black pebbles"). Crusts are accompanied by oncoidal wackestones with Bacinella-Lithocodium oncoids. C/adocorops/s-cayeuxiid floatstones are transitional to the facies of the coral patch reef belt. Seaward of the coral patch reef belt, bioclastic and oolitic sands occupy the proximal middle ramp. The transition to deeper water is reflected by changes in sedimentary and faunal composition from moderately to poorly sorted bioclastic and intraclastic grainstones/rudstones, to oolitic sands, and eventually to fine grained bioclastic packstones. In these packstone areas, coral reef banks grew which are entirely different from coral reefs of the patch reef belt. They were constructed almost exclusively by thin laminoid fungiid corals (Microsolena sp., Comoseris sp. Thamnasteria sp.). Seaward adjacent to these packstone areas are sponge meadows with interspersed microbialite/siliceous sponge reefs. These are followed by monotonous bioclastic wackestones. Small mud mounds bearing siliceous sponge are intercalated. The different reef types occupied specific positions on the ramp. In general spongiolitic facies developed at a more distal and deeper position on the ramp than any coral-dominated facies. The development of the carbonate ramp started with a rapid transgression in Lower Oxfordian time. At the end of the transgressive phase sponge meadows could establish themselves at water depths below about 25 m. During the time of relative sea level high stand microbialite-siliceous sponge bioherms developed, interspersed into the sponge meadows. These spongiolitic reefs occasionally show peculiar ring shapes, a feature that is only observed in Romania. Their formation was most probably controlled by a preexisting uneven surface with subtle hollows. The spongiolitic bioherms had an early cemented microbialitic framework, which was settled by lithistid demosponges and hexactinellid sponges. After the death of the sponges, their skeletons were also calcified and microbially cemented. The ring-shaped bioherms developed on the distal middle ramp below fair weather wave base, where only during heavy storms waves could touch the bottom. On the outer ramp below storm wave base small thrombolitic mud mounds dominated by hexactinellid sponges developed at the same time. Landwards, on the middle ramp, the spongiolitic belt interfingered with bioclastic sands. In water depths of about 1 0 to 1 5 m very thin platy corals appeared forming wide biostromes (fungiid biostromes). One important reason why hermatypic corals did not substitute the siliceous sponge facies in deeper water as well might have been pulses of slightly elevated nutrient concentrations. These elevated nutrient concentrations stimulated growth of plankton, which reduced water transparency, limiting depth range of hermatypic corals and calcareous algae. On the other hand high water turbulence together with elevated rates of sediment input and sediment movement prevented siliceous sponges from growing in areas where fair weather waves influenced the sea-bottom. Regression started in late Oxfordian time and lagoonal and bioclastic facies of the inner ramp prograded to the west. During this phase coral patch reefs developed in very shallow and turbulent water and coral-stromatoporoid patch reefs grew on the proximal middle ramp. The microbialite-siliceous sponge association first disappeared in the eastern part of the Central Dobrogea. In the western part the spongiolitic association was substituted by coral-dominated associations only during the latest Oxfordian. All reef types bearing microbialites (all spongiolitic buildups and fungiid biostromes) developed during transgression or relative sea level highstand. Coral patch reefs in shallow water did establish themselves during the regressive phase. Two basic types of microbialite crusts are recognized in Central Dobrogea: Fenestral automicritic crusts and peloidal automicritic crusts. In fenestral automicritic crusts lamination is often indistinct and defined by dense intervals alternating with losely packed intervals where small linear arranged spar-cemented areas (fenestrae) occur. This crust type is exclusively observed in the spongiolitic belt on the outer ramp where it forms the primary 'framework' in the thrombolitic mudmounds and participates in the hexactinellid-dominated biostromes. In a slightly shallower position within the ring-shaped bioherms they play only a minor role. Peloidal automicritic crusts show a rhythmical lamination which originates from the alternation of spar-cemented peloidal intervals and thin micritic layers. The peloidal intervals have integrated a varying amount of detrital grains. A fine-grained variety of this crust type forms the rigid primary framework of the ring-shaped bioherms. Coarse-grained varieties, locally with an ooid portion, developed in somewhat shallower and more turbulent water in the fungiid biostromes and in the coral-stromatoporoid patch reefs. Like the formation of the different crust types, the early diagenesis of sponge skeletons together with their organic tissue is another example for a microbially induced formation of automicrites. In general two modes of cementation are distinguished, a dense aphanitic and a peloidal one. It is assumed that the mode of cementation of the siliceous sponges (lithistid demosponges and hexactinellids) depends on the taxonomic affiliation of the sponges and on the physical and chemical conditions of the environment where they lived and died. Lithistid demosponges always show a peloidal mode of preservation. Hexactinellids, from deep and very low energy settings, however, exhibit dense aphanitic cementation and complete preservation. In shallower, more turbulent zones (ring-shaped bioherms) they have a low preservation potential and are in general incompletely preserved with a coarse grained peloidal mode of cementation.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; ddc:554 ; Paläobiologie
    Language: German
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  • 14
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    Miscellanea Palaeontologica 5 (1996)
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    Details
    Publication Date: 2024-04-17
    Description: Baron-Szabo, R.C. & Steuber, T.: Korallen und Rudisten aus dem Apt im tertiären Flysch des Pamass-Gebirges bei Delphi-Arachowa (Mittelgriechenland) … 3 ; Fechner, G.G.: Septarienton und Stettiner Sand als Fazieseinheiten im Rupelium der östl. Mark Brandenburg: Palynologisch-fazielle Untersuchungen bei Bad Freienwalde ... 77 ; Fischer, K.: Das Mammut (Mammuthus primigenius Blumenbach, 1799) von Klinge bei Cottbus in der Niederlausitz (Land Brandenburg) ... 121 ; Frydas, D. & Keupp, H.: Biostratigraphical results in Late Neogene deposits of NW Crete, Greece, based on calcareous nannofossils ... 169 ; Kohring, R.: Structure and Biomineralization of Eggshell of Elaphe guttata (Linnö 1766) (Serpentes: Colubridae) ... 191 ; Kriiger, F.J.: Parietale Modifikationen bei Echinocorys obliqua (Nilssohn 1828) (Echinoidea, Holasterida) und ihre Beziehungen zur Weichkörper-Organisation ... 201 ; May, A. & Becker, R.T.: Ein Korallen-Horizont im Unteren Bänderschiefer (höchstes Mitteldevon) von Hohenlimburg-Elsey im Nordsauerland (Rheinisches Schiefergebirge) ... 209 ; Mehl, D. & Reitner, J.: Observations on Astraeospongium meniscum (Roemer, 1848) from the Silurian of western Tennessee: Constructional morphology and palaeobiology of the Astraeospongiidae (Calcarea, Heteractinellidae) 243 ; Neumann, C.: The mode of life and paleobiogeography of the genus Douvillaster Lambert (Echinoidea: Spatangoida) as first recorded in the Lower Cretaceous (Albian) of Spain ... 257 ; Niebuhr, B.: Die Scaphiten (Ammonoidea, Ancyloceratina) des höheren Obercampan der Lehrter Westmulde östlich Hannover (N-Deutschland) ... 267 ; Rehfeld, U.: Der Ausgangschemismus fossiler peloidaler und aphanitischer Zemente - eine geochemische Analyse an jurassischen und kretazischen Karbonatgesteinen ... 289 ; Rehfeld, U.: Steuerungsfaktoren bei der Dissoziierung des Skelettes und der Zementation des Gewebes bei jurassischen und kretazischen Kieselschwämmen ... 303 ; Rehfeld, U.: Paläoredoxpotential während der Diagenese von jurassischen und kretazischen spongiolithischen Biokonstruktionen ... 321 ; Werner, C. & Bardet, N.: New record of elasmosaurs (Reptilia, Plesiosauria) in the Maastrichtian of the Western Desert of Egypt ... 335 ; Wiese, F.: Preliminary Data on the Turanian Ammonite Biostratigraphy of the Liencres Area (Province Cantabria, Northern Spain) ... 343 ; Wilmsen, M.: Flecken-Riffe in den Kalken der „Formaciön de Altamira“ (Cenoman, Cobreces/Tofianes-Gebiet, Prov. Kantabrien, Nord-Spanien): Stratigraphische Position, fazielle Rahmenbedingungen und Sequenzstratigraphie ... 353 ; Rauhut, O.W.M.: Bibliographie 1995, Institut für Paläontologie, Freie Universität Berlin ... 375 ;
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Paläobiologie ; Paläontologie
    Language: German , English
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  • 15
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    Wasserpflanzengesellschaften und Moore in Uruguay (1983)
    In:  SUB Göttingen | ZA 34278
    Details
    Publication Date: 2024-03-07
    Description: Im Nordosten von Uruguay wurden Wasserpflanzengesellschaften und Niedermoore untersucht. Flache Tümpel werden von Pflanzengesellschaften besiedelt, in denen Jussiaea repens, Nymphoides humboldtiana, Hydrocleis nymphoides und Echinodurus andrieuxii dominieren. Zusätzlich gibt es Gewässer mit ausgedehnten Azolla-Beständen. In der Talaue des Rocha-Flusses finden sich Quellmoore, die von einer hochwüchsigen Cyperacee (Androtrichum giganteum) geprägt werden. Manche küstennahen Dünentäler sind mit Niedermooren ausgefüllt, deren Vegetation physiognomisch an Kleinseggenrieder erinnert. Dort finden sich Eleocharis sellowiana, Paspalum pumilum, Triglochin montevidense und eingestreut auch Juncus acutus.
    Description: In the northeast of Uruguay plant associations of fens and flat puddles have been examined. The puddles in the pampa are colonized by plant associations with Jussiaea repens, Nymphoides humboldtiana, Hydrocleis nymphoides‚and Echinodurus andrieuxii. In addition there are ponds which are extended Azolla-habitats. Spring-water fens appear in the water meadows of the Rocha-river. They are dominated by a sedge species, named Androtrichum giganteum. Between the coastel dunes fens grow up, which remind of the Parvo-Caricetum in the northern hemisphere. There Eleocharis sellowiana, Paspalum pumilum, Triglochin montevidense and occasionally Juncus acutus are found.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:581.7 ; Moor ; Torf ; Vegetation ; peatland ; peat
    Language: German
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  • 16
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    Hinweise auf Bücher zum Thema »Moor und Torf« (1983)
    In:  SUB Göttingen | ZA 34278
    Details
    Publication Date: 2024-03-07
    Description: bibliography
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:581.7 ; ddc:333.72 ; ddc:630.914 ; Moor ; Torf ; Rezension ; peatland ; peat
    Language: German
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  • 17
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    Hinweise auf Bücher zum Thema „Moor und Torf” (1996)
    In:  Herausgeberexemplar
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    Publication Date: 2024-03-21
    Description: abstract
    Description: DFG, SUB Göttingen
    Keywords: Rezension
    Language: German
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  • 18
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    Göttinger Bodenkundliche Berichte 76 (1983)
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Details
    Publication Date: 2024-05-20
    Description: research
    Keywords: Bioelementbilanzen ; Transport ; Sand-Lysimetern ; Grundwasserständen
    Language: German
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  • 19
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    Göttinger Bodenkundliche Berichte 78 (1983)
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Details
    Publication Date: 2024-05-20
    Description: research
    Keywords: Eutrophierung ; Düngemittel ; Bodenschutz ; Nährstoffauswaschung ; Stoffübertragung ; Phosphathaushalt ; Saurer Boden
    Language: German
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  • 20
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    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
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  • 21
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    A cellular automaton for the development of crustal shear zones (1996)
    In:  Tectonophys., Luxembourg, EGS-Gauthier-Villars, vol. 253, no. 2, pp. 247-270, pp. 2324
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    Publication Date: 1996
    Keywords: Fault zone ; Statistical investigations ; Fracture
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  • 22
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    Implications of selected subsurface data on the structural form and evolution of some basins in the northern Basin and Range province, Nevada and Utah (1983)
    In:  Geol. Soc. Am. Bull., Luxembourg, EGS-Gauthier-Villars, vol. 94, no. 2, pp. 1055-1072, pp. L23608
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    Publication Date: 1983
    Keywords: Tectonics ; rifting ; USA ; Geol. aspects ; Stress ; GSA
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  • 23
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    A statistical approach to the extraction of the seismic propagation wavelet (1983)
    In:  Geophys. Prosp., Luxembourg, EGS-Gauthier-Villars, vol. 31, no. 2, pp. 726-747, pp. L23303
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    Publication Date: 1983
    Keywords: Wavelet processing ; Inversion
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  • 24
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    Spec. iss.: Tsunamis impacting on the European coasts: modelling, observation and warning (1996)
    In:  Physics and Chemistry of the Earth, Warszawa, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 21, no. 1-2, 92 pp., pp. 1969-1986, pp. 2121
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    Publication Date: 1996
    Keywords: Tsunami(s) ; Proceedings of a conference ; Early warning systems (earthquakes, volcanic eruptions, tsunamis etc.) ; TWS ; Modelling ; Data analysis / ~ processing ; Real time earthquake monitoring ; BIBTEX?
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  • 25
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    Permeability and stress in crystalline rocks (1996)
    In:  Terra Nova, Warszawa, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 8, no. 3, pp. 223-235, pp. 2121
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    Keywords: Stress ; Physical properties of rocks
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  • 26
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    The initiation of the Dead Sea rift (1983)
    In:  J. of Geology, Washington D.C., Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 91, no. 1-2, pp. 307-321, pp. L08305
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    Publication Date: 1983
    Keywords: Plate tectonics ; Geol. aspects ; Fault zone
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  • 27
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    Tilt and seismicity changes in the Shumagin seismic gap (1983)
    In:  Science, Leiden, Noordhoff, vol. 222, no. 3, pp. 322-325, pp. 1892
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    Keywords: Earthquake precursor: prediction research
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  • 28
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    Three-dimensional P and S wave velocity structure of Redoubt Volcano, Alaska (1996)
    In:  J. Geophys. Res., San Francisco, Pergamon, vol. 101, no. 20, pp. 8111-8128, pp. 1246
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    Publication Date: 1996
    Keywords: Three dimensional ; P-waves ; Shear waves ; Velocity depth profile ; Volcanology ; JGR
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  • 29
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    The accuracy of soil response estimates using soil-to-rock spectral ratios (1996)
    In:  Bull. Seism. Soc. Am., San Francisco, Pergamon, vol. 86, no. 2, pp. 519-523, pp. 1246
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    Publication Date: 1996
    Keywords: Site amplification ; Spectrum ; Error analysis ; BSSA
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  • 30
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    Global Positioning System measurements to constrain geodynamic processes in Fennoscandia (1996)
    In:  Eos, Trans., Am. Geophys. Un., Warszawa, Elsevier, vol. 77, no. 35, pp. 337, 341, pp. L21303, (ISBN: 0-12-018847-3)
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    Publication Date: 1996
    Keywords: Geodesy ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; post-glacial ; uplift ; Project report/description
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  • 31
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    Interpolation of principal stress directions by nonparametric statistics: Global maps with confidence limits (1996)
    In:  J. Geophys. Res., Warszawa, Elsevier, vol. 101, no. 2, pp. 5435-5444, pp. L02307, (ISBN: 0-12-018847-3)
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    Publication Date: 1996
    Keywords: Stress ; Statistical investigations ; Data analysis / ~ processing ; Plate tectonics ; JGR
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  • 32
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    The western margin of the Bohemian Massif in Bavaria (1983)
    In:  Fortschr. Miner., Warszawa, Elsevier, vol. 61, no. 22, pp. 171-195, pp. L11309, (ISBN: 0-12-018847-3)
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    Keywords: KTB ; Geol. aspects ; Bluemel ; Blumel
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  • 33
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    Orientation of the stress field from breakouts in a crystalline well in a seismic active area (1983)
    In:  Phys. Earth Plan. Int., Warszawa, Elsevier, vol. 33, no. 22, pp. 250-254, pp. L11309, (ISBN: 0-12-018847-3)
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    Publication Date: 1983
    Keywords: Stress ; Stress measurements ; Seismicity ; Borehole breakouts ; Bluemling ; Blumling ; PEPI
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  • 34
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    Some applications of pattern recognition to oil and gas exploration (1983)
    In:  IEEE Transaction on Geoscience and Remote Sensing, Warszawa, Elsevier, vol. GE-21, no. 4, pp. 416-426, pp. B02309, (ISBN: 0-12-018847-3)
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    Publication Date: 1983
    Keywords: Discrim. anal. ; Pattern recognition ; Seismic stratigraphy
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  • 35
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    Viscoelastic stress relaxation on deep fault sections as a possible source of very long period waves (1983)
    In:  J. Geophys. Res., Taipei, Elsevier, vol. 88, no. 7, pp. 2251-2260, pp. 2091, (ISBN: 0-12-018847-3)
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    Publication Date: 1983
    Keywords: Inelastic ; Chandler wobble ; Seismology ; Stress ; JGR
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    Fault slip beyond a barrier on a transform plate boundary (1983)
    In:  Geophys. J. R. astr. Soc., Taipei, Elsevier, vol. 75, no. 7, pp. 143-154, pp. 2091, (ISBN: 0-12-018847-3)
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    Keywords: Earthquake barriers ; Dislocation ; Plate tectonics ; GJRaS
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  • 37
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    Seismic response of a hill: the example of Tarzana, California (1996)
    In:  Bull. Seism. Soc. Am., Leipzig, Birkhäuser Verlag, vol. 86, no. 6, pp. 66-72, pp. 2366, (ISBN: 0-12-018847-3)
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    Publication Date: 1996
    Keywords: Site amplification ; Strong motions ; Finite difference method ; USA ; Waves ; Seismology ; accelerations ; topography ; BSSA
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  • 38
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    Vertical seismic profile results from the Kola superdeep borehole, Russia (1996)
    In:  Tectonophysics, Luxembourg, Conseil de l'Europe, vol. 264, no. 1-4, pp. 295-308, pp. B04313, (ISBN: 0-12-018847-3)
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    Keywords: Borehole geophys. ; scientific drilling ; Vertical seismic profiling ; EUROPROBE (Geol. and Geophys. in eastern Europe) ; SG3
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  • 39
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    Focal depths of intracontinental earthquakes and their implications for the thermal and mechanical properties of the lithosphere (1983)
    In:  J. Geophys. Res., Taipei, Conseil de l'Europe, vol. 88, no. 3, pp. 4183-4214, pp. B09401, (ISBN: 0-12-018847-3)
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    Keywords: Lithosphere ; Earthquake ; Hypocentral depth ; Geothermics ; Physical properties of rocks ; JGR
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  • 40
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    Distribution of angular misfits in fault-slip data (1996)
    In:  Journal of Structural Geology, Taipei, Elsevier, vol. 18, no. 11, pp. 1353-1367, pp. TC1002, (ISBN: 0-12-018847-3)
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    Keywords: paleo ; Stress ; Geol. aspects ; Structural geology ; JSG
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  • 41
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    Velocity filtering of seismic reflection data (1983)
    In:  First Break, Taipei, Elsevier, vol. 1, no. 7-8, pp. 9-24, pp. RG2001, (ISBN: 0-12-018847-3)
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    Keywords: Reflection seismics ; Filter- ; Velocity analysis ; Seismics (controlled source seismology)
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    Complexity of seismicity due to highly rate-dependent fiction (1996)
    In:  J. Geophys. Res., Heidelberg, 3-4, vol. 101, no. 11, pp. 25,321-25,336, pp. 1516, (ISBN: 0-12-018847-3)
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    Keywords: Seismicity ; Friction ; Seismology ; JGR
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  • 43
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    Time-dependent uplift of the Kenai Peninsula and adjacent regions of south central Alaska since the 1964 Prince William Sound earthquake (1996)
    In:  J. Geophys. Res., Heidelberg, North Holland Publishing Company, vol. 101, no. 4, pp. 8595-8604, pp. 1516, (ISBN: 0-12-018847-3)
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    Publication Date: 1996
    Keywords: Inelastic ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Earthquake ; JGR
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  • 44
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    Observation of shallow anisotropy on local earthquake records at the Garner valley, southern California, downhole array (1996)
    In:  Bull. Seism. Soc. Am., Roma, Acad. Roy. des Sciences, vol. 86, no. 1, pp. 477-488, pp. B04102, (ISBN: 0-12-018847-3)
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    Keywords: Anisotropy ; Local earthquakes ; Borehole geophys. ; USA ; Seismic arrays ; Seismology ; anisotropy ; southern ; California ; BSSA
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    Realistic inversions to obtain gross properties of the earthquake faulting process (1996)
    In:  Tectonophysics, Warszawa, Army Corps of Engineers, Woodward-Clyde Consultants, vol. 261, no. 1-3, pp. 165-178, pp. B05310, (ISBN: 0-12-018847-3)
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    Keywords: Inversion ; Fracture ; Source
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    Why large earthquakes do not nucleate at shallow depths (1983)
    In:  Nature, Warszawa, Army Corps of Engineers, Woodward-Clyde Consultants, vol. 305, no. 36, pp. 621-623, pp. B05310, (ISBN: 0-12-018847-3)
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    Publication Date: 1983
    Keywords: Seismology ; Source parameters ; Earthquake asperities ; CRUST ; Hypocentral depth
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    On the inverse problem for earthquake rupture: The Haskell-type source model (1996)
    In:  J. Geophys. Res., Warszawa, Army Corps of Engineers, Woodward-Clyde Consultants, vol. 101, no. 1-3, pp. 5725-5738, pp. B05310, (ISBN: 0-12-018847-3)
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    Keywords: Fracture ; Source ; Seismology ; JGR
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    Infinite boundary elements for the analysis of halfspace problems (1996)
    In:  Computers and Geotechnics, London, Army Corps of Engineers, Woodward-Clyde Consultants, vol. 19, no. 2, pp. 137-151, pp. 1013, (ISBN: 0-12-018847-3)
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    Keywords: Modelling ; Boundary Element Method ; Elasticity
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    RMS response of a one-dimensional half-space to SH (1996)
    In:  Bull. Seism. Soc. Am., London, Army Corps of Engineers, Woodward-Clyde Consultants, vol. 86, no. 2, pp. 363-370, pp. 1013, (ISBN: 0-12-018847-3)
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    Keywords: Site amplification ; Modelling ; SH waves ; noksp ; BSSA
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    Elastic stress relaxation: A mechanism for opposite sense of secondary faulting with respect to a major fault (1996)
    In:  Tectonophysics, Luxembourg, Pergamon, vol. 257, no. 2-4, pp. 175-188, pp. 2131, (ISBN 1-86239-117-3)
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    Keywords: Stress ; Geol. aspects ; Physical properties of rocks ; Fracture
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    Exhumation of the Dabie Shan ultrahigh-pressure rocks (1996)
    In:  Geowissenschaften, Amsterdam, Elsevier, vol. 14, no. 7-8, pp. 308-309, pp. 2083, (ISBN 1-86239-117-3)
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    Keywords: Tectonics ; metamorphic ; China ; scientific drilling ; Geol. aspects
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    Seismic tomography and deformation modeling of the junction of the San Andreas and Calaveras faults (1996)
    In:  J. Geophys. Res., London, Elsevier, vol. 101, no. 8, pp. 27,917-27,942, pp. 2083, (ISBN 1-86239-117-3)
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    Keywords: Tomography ; Fault zone ; triple ; junction ; Modelling ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; JGR
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    Quaternary state of stress in the Northern Andes and the restraining bend model for the Ecuadorian Andes (1996)
    In:  Tectonophysics, Münster, Amer. Sc., vol. 259, no. 3, pp. 101-116, pp. 1228, (ISBN 0-471-26610-8)
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    Keywords: Stress ; paleo ; Plate tectonics ; Structural geology ; Sebrier
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    Seismic anisotropy within the uppermost mantle of southern Germany (1996)
    In:  Geophys. J. Int., Münster, 3, vol. 125, no. 3, pp. 747-767, pp. L11308, (ISBN 0-471-26610-8)
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    Keywords: AnisotropyS ; Teleseismic events ; GJI
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    Deadly quake (1996)
    In:  Eos, Trans., Am. Geophys. Un., Münster, 3, vol. 77, no. 7, pp. 62, pp. L12311, (ISBN 0-471-26610-8)
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    Keywords: Earthquake ; China ; AGU
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    Live load induced vibrations in Ullevi stadium -- dynamic soil analysis (1996)
    In:  Soil Dynamics and Earthquake Engineering, Luxembourg, Am. Soc. Mech. Eng., vol. 15, no. 3, pp. 171-188, pp. L12311, (ISBN 0-471-26610-8)
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    Publication Date: 1996
    Keywords: Earthquake engineering, engineering seismology ; Finite Element Method ; Modelling ; soft ; high-plastic ; clay ; soil ; dynamics ; finite ; element ; analysis ; Rayleigh ; damping ; hysteretic ; damping ; case ; history ; rock ; music ; induced ; vibrations ; noksp ; Gothenburg ; Sweden ; SDEE
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    A teleseismic-specific detection algorithm for single short-period traces (1983)
    In:  Bull. Seism. Soc. Am., Luxembourg, Am. Soc. Mech. Eng., vol. 73, no. 11, pp. 1173-1186, pp. L12311, (ISBN 0-471-26610-8)
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    Keywords: Teleseismic events ; Detectors ; Spectrum ; Spectral analysis ; High frequency ... ; BSSA
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    Type of faulting and orientation of stress and strain as a function of space and time in Kilauea's south flank, Hawaii (1996)
    In:  J. Geophys. Res., Bonn, South Afr. Inst. Mining Metall., vol. 101, no. 1, pp. 16,025-16,042, pp. 1056, (ISBN: 0534351875, 2nd edition)
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    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Volcanology ; Stress ; Fracture ; JGR
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    Tectonic stress within the New Madrid seismic zone (1996)
    In:  J. Geophys. Res., Warszawa, Icelandic Meteorological Office, Ministry for the Environment,, vol. 101, no. 4, pp. 5445-5458, pp. 2540, (ISBN: 0534351875, 2nd edition)
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    Keywords: Stress ; Tectonics ; Plate tectonics ; intra-plate ; JGR
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    Simulating seismic wave propagation in 3D elastic media using staggered-grid finite diferences (1996)
    In:  Bull. Seism. Soc. Am., Warszawa, Icelandic Meteorological Office, Ministry for the Environment,, vol. 86, no. 4, pp. 1091-1106, pp. L05602, (ISBN: 0534351875, 2nd edition)
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    Keywords: Finite difference method ; Three dimensional ; Modelling ; BSSA ; SRICHWALSKI
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    Finite-element modelling of stress patterns along the Mid-Norwegian continental margin, 62° to 68° N (1996)
    In:  Tectonophys., Bonn, Pergamon, vol. 266, no. 1-4, pp. 33-53, pp. 2144, (ISBN: 0534351875, 2nd edition)
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    Keywords: Stress ; Finite Element Method ; Modelling ; Borehole geophys. ; Borehole breakouts ; Fault plane solution, focal mechanism ; Golke
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    Origins of the European regional stress field (1996)
    In:  Tectonophys., Bonn, Pergamon, vol. 266, no. 1-4, pp. 11-24, pp. 2144, (ISBN: 0534351875, 2nd edition)
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    Publication Date: 1996
    Keywords: Stress ; Finite Element Method ; Modelling ; EUROPROBE (Geol. and Geophys. in eastern Europe) ; World Stress Map (Project) ; one ; degree ; resolution ; Golke ; FROTH ; (abstract)
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  • 63
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    Orientation of crustal stresses in the North Sea and Barents Sea inferred from borehole breakouts (1996)
    In:  Tectonophys., Bonn, Pergamon, vol. 266, no. 1-4, pp. 25-32, pp. 2144, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1996
    Keywords: Stress ; Finite Element Method ; Modelling ; Borehole geophys. ; Borehole breakouts ; Golke
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  • 64
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    Stress fields controlling strike-slip faulting in Iceland (1996)
    Pergamon
    In:  Physics and Chemistry of the Earth, London, Pergamon, vol. 21, no. 4, pp. 261-265, pp. B05401, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1996
    Keywords: Stress ; Geol. aspects ; Modelling ; cracks and fractures (.NE. fracturing) ; Fault zone ; Plate tectonics ; Strike-slip ; Modelling
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  • 65
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    Off-rift and rift-zone palaeostresses in Northwest Iceland (1996)
    In:  Tectonophysics, London, Pergamon, vol. 255, no. 3-4, pp. 211, pp. B05401, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1996
    Keywords: paleo ; Stress ; Geol. aspects ; Tectonics ; Plate tectonics
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  • 66
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    A gap is ... (1983)
    In:  Bull. Seism. Soc. Am., Warszawa, Eötvös Lorand Geophysical Institute of Hungaria, vol. 73, no. B7, pp. 1485-1486, pp. 2342, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1983
    Keywords: Earthquake precursor: prediction research ; BSSA
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  • 67
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    Crustal-scale extension in the central Pannonian basin (1996)
    In:  Tectonophysics, Basel, Birkhäuser Verlag, vol. 264, no. 1-4, pp. 191-204, pp. B05S07, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1996
    Keywords: EUROPROBE (Geol. and Geophys. in eastern Europe) ; rifting ; Deep seismic sounding (espec. cont. crust) ; Muller
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  • 68
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    Butterworth dip filters (wavelet) (1983)
    In:  Geophysics, Basel, Birkhäuser Verlag, vol. 48, no. 6-7, pp. 1033-1038, pp. B05S07, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1983
    Keywords: Filter- ; Wavelet processing
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  • 69
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    A probability model for earthquake prediction (1983)
    In:  Earthq. Predict. Res., Basel, Birkhäuser Verlag, vol. 2, no. 4, pp. 227-234, pp. B05S07, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1983
    Keywords: JAPAN ; Earthquake precursor: prediction research ; Seismicity ; Earthquake precursor: statistical anal. of seismicity
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  • 70
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    Tectonic interpretation of enigmatic structures in the North Anatolian fault zone (1983)
    In:  J. Struct. Geol., Luxembourg, Conseil de l'Europe, vol. 5, no. 5787, pp. 217-220, pp. B05S07, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1983
    Keywords: Geol. aspects ; Turkey ; Fault zone ; NAF ; Structural geology ; Stress ; Çerkes ; Cerkes ; Erbaa ; ova ; JSG
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  • 71
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    The structural evolution of the NE Atlantic region (1983)
    In:  Geologisches Jahrbuch, Luxembourg, Conseil de l'Europe, vol. B52, no. 7055, pp. 3-37, 15 figs, 1 tab., pp. B05S07, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1983
    Keywords: Review article ; Plate tectonics ; Geol. aspects
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  • 72
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    Initial-value and modal approaches for transient viscoelastic responses with complex viscosity profiles (1996)
    In:  Geophys. J. Int., Luxembourg, Conseil de l'Europe, vol. 127, no. 3-4, pp. 348-362, pp. L17606, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1996
    Keywords: Rheology ; Inelastic ; NOModelling ; Earth rotation ; (The Earth's free) oscillations ; GJI
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  • 73
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    Determination of the isotropic component of deep focus earthquakes by inversion of normal-mode data (1996)
    In:  Geophys. J. Int., Luxembourg, Conseil de l'Europe, vol. 127, no. 3, pp. 515-528, pp. L17606, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1996
    Keywords: Moment tensor ; Inversion ; NOModelling ; GJI
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  • 74
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    Eustasy as a test of a Cretaceous superplume hypothesis (1996)
    In:  Earth planet. Sci. Lett., Luxembourg, Conseil de l'Europe, vol. 137, no. 2, pp. 101-108, pp. L17606, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1996
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geol. aspects ; Plate tectonics
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  • 75
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    Das Erdbeben bei Ibbenbüren am 13. Juli 1981 (1983)
    In:  Geol. Jb., Hannover, Conseil de l'Europe, vol. E26, no. 31, pp. 65-76, pp. B04310, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1983
    Keywords: Rock bursts (see also ERDSTOSS and GEBIRGSSCHLAG) ; ERDSTOSS (see also rockburst and Gebirgsschlag)
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  • 76
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    In the shadow of 1857: The effect of the great Fort Tejon earthquake on subsequent earthquake in southern California (1996)
    In:  Geophys. Res. Lett., Münster, Inst. f. Geophys., Ruhr-Univ. Bochum, vol. 23, no. 3, pp. 229-232, pp. B04310, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1996
    Keywords: Seismology ; history ; Earthquake ; GRL
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  • 77
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    Inversion of strong ground motion and teleseismic waveform data for the fault rupture history of the 1979 Imperial Valley, California, earthquake (1983)
    In:  Bull. Seism. Soc. Am., Münster, 3, vol. 73, no. 6, pp. 1553-1583, pp. L23301, (ISBN: 0534351875, 2nd edition)
    Details
    Publication Date: 1983
    Keywords: Seismology ; Inversion ; Strong motions ; Earthquake ; Teleseismic events ; BSSA
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  • 78
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    Individual faults can't produce a Gutenberg-Richter earthquake recurrence (1996)
    In:  Engineering Geology, Stuttgart, Conseil de l'Europe, vol. 43, no. 1, pp. 5-9, pp. L17311, (ISSN 0343-5164)
    Details
    Publication Date: 1996
    Keywords: Earthquake hazard ; Earthquake engineering, engineering seismology ; Seismicity ; Gutenberg-Richter magnitude frequency b-value ; characteristic ; earthquake ; Recurrence of earthquakes ; Statistical investigations ; ENGGL
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  • 79
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    Stress-induced late-stage subsidence anomalies in the Pannonian basin (1996)
    In:  Tectonophys., Tokyo Univ., Geophys. Inst., Fac. of Science, vol. 266, no. 1-4, pp. 287-300, pp. L23611, (ISSN 0343-5164)
    Details
    Publication Date: 1996
    Keywords: Stress ; EUROPROBE (Geol. and Geophys. in eastern Europe) ; Geol. aspects ; paleo
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  • 80
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    The mechanical properties of materials with interconnected cracks and pores (1996)
    In:  Geophys. J. Int., Taipei, Am. Inst. Min. Metal. Petr. Eng., vol. 124, no. 2, pp. 105-112, pp. 2324, (ISSN 0343-5164)
    Details
    Publication Date: 1996
    Keywords: AnisotropyS ; Physical properties of rocks ; cracks and fractures (.NE. fracturing) ; GJI
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  • 81
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    Source process of the 1995 Kobe earthquake: Detemination of spatio-temporal slip distribution by Bayesian modeling (1996)
    In:  Bull. Seism. Soc. Am., Stuttgart, Schweizerbart'sche Verlagsbuchhandlung, vol. 86, no. 2, pp. 547-566, pp. 2077, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1996
    Keywords: Earthquake ; Japan ; Modelling ; Source ; Seismology ; BSSA
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  • 82
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    Transient creep of a composite lower crust, 2, A polymineralic basis for rapidly evolving postseismic deformation modes (1996)
    In:  J. Geophys. Res., Amsterdam, Schweizerbart'sche Verlagsbuchhandlung, vol. 101, no. 1-4, pp. 28,005-28,028, pp. L09302, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1996
    Keywords: Rheology ; Creep observations and analysis ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; JGR
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  • 83
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    Hypothesis testing and earthquake prediction (1996)
    In:  Proceedings of the National Academy of Sciences of the USA, Amsterdam, Schweizerbart'sche Verlagsbuchhandlung, vol. 93, no. 4, pp. 3830-3837, pp. L07302, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1996
    Keywords: Statistical investigations ; Seismicity ; Earthquake precursor: prediction research ; Data analysis / ~ processing ; cycles
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  • 84
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    Evolution of moderate seismicity in the San Francisco Bay region, 1850 to 1993 (1996)
    In:  J. Geophys. Res., Berlin, Schweizerbart'sche Verlagsbuchhandlung, vol. 101, no. 11/12, pp. 765-790, pp. L07302, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1996
    Keywords: Seismicity ; Statistical investigations ; JGR
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  • 85
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    Phase transitions and mantle discontinuities (1983)
    In:  Rev. Geophys. Space Phys., Berlin, Schweizerbart'sche Verlagsbuchhandlung, vol. 21, no. 1-2, pp. 51-74, pp. L07302, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1983
    Keywords: Review article ; Earth model, also for more shallow analyses ! ; Geochemistry ; Mineralogy ; Seismology
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  • 86
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    Nonlinear elasticity and stress-induced anisotropy in rock (1996)
    In:  J. Geophys. Res., San Francisco, Schweizerbart'sche Verlagsbuchhandlung, vol. 101, no. 8, pp. 3113-3124, pp. B10404, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1996
    Keywords: Non-linear effects ; Anisotropy ; Stress ; Physical properties of rocks ; JGR
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  • 87
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    Seismic moment assessment of earthquakes in stable continental regions - 3. New Madrid 1811-1812, Charleston 1886 and Lisbon 1755 (1996)
    In:  Geophys. J. Int., San Francisco, Schweizerbart'sche Verlagsbuchhandlung, vol. 126, no. 1, pp. 314-344, pp. TC1011, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1996
    Keywords: Seismicity ; intraplate ; seismic Moment ; Plate tectonics ; GJI
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  • 88
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    Andean tectonics related to geometry of subducted Nazca plate (1983)
    In:  Geological Study of America Bulletin, Reykjavík, Icelandic Meteorological Office, Ministry for the Environment University of Iceland, vol. 94, no. 5, pp. 341-361, pp. TC1011, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1983
    Keywords: Plate tectonics ; Subduction zone ; South
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  • 89
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    Ghosting and marine signature deconvolution - a prerequisite for a detailed seismic interpretation (1983)
    In:  Geophysics, (submitted), Icelandic Meteorological Office, Ministry for the Environment University of Iceland, vol. 48, no. 1-2, pp. 1468-1485, pp. TC1011, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1983
    Keywords: Deconvolution
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  • 90
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    Reappraisal of deep seismic reflection Profile VIII across the Pripyat Trough (1996)
    In:  Tectonophys., (submitted), Icelandic Meteorological Office, Ministry for the Environment University of Iceland, vol. 268, no. 19, pp. 99-108, pp. TC1011, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1996
    Keywords: EUROPROBE (Geol. and Geophys. in eastern Europe) ; rift ; Deep seismic sounding (espec. cont. crust) ; Reflection seismics ; paleo ; Tectonics ; seismic Migration ; CRUST ; Moho
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  • 91
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    Evidence for dyke intrusion earthquake mechanisms near Long Valley, California (1983)
    In:  Nature, London, Icelandic Meteorological Office, Ministry for the Environment University of Iceland, vol. 303, no. 1, pp. 323-325, pp. TC1011, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1983
    Keywords: Seismology ; Volcanology ; Fault plane solution, focal mechanism ; CLVD ; USA
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  • 92
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    The effect of deglaciation on mantle melting beneath Iceland (1996)
    In:  J. Geophys. Res., London, Icelandic Meteorological Office, Ministry for the Environment University of Iceland, vol. 101, no. 4, pp. 21,815-21,828, pp. TC1011, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1996
    Keywords: Rheology ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; JGR
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  • 93
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    Radiation and receiver patterns of shear and compressional waves as a function of Poisson's ratio (1983)
    In:  Geophys. Prosp., London, Icelandic Meteorological Office, Ministry for the Environment University of Iceland, vol. 31, no. 3, pp. 421-435, pp. B02206, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Details
    Publication Date: 1983
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  • 94
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    Triple seismic zone and the regional variation of seismicity along the northern Honshu arc (1983)
    In:  J. Geophys. Res., Amsterdam, Univ. Tokyo, vol. 88, no. 3, pp. 4215-4230, pp. L14309, (ISSN: 1340-4202)
    Details
    Publication Date: 1983
    Keywords: Seismicity ; Subduction zone ; Japan ; Hypocentral depth ; Seismology ; JGR
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  • 95
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    How does the shear-wave structure of the seabed affect the seismic wavefield? (1996)
    In:  Geophys. J. Int., New York, Allerton Press, vol. 124, no. 19, pp. 341-348, pp. L01606, (ISSN: 1340-4202)
    Details
    Publication Date: 1996
    Keywords: Shear waves ; Velocity depth profile ; Waves ; Seismics (controlled source seismology) ; Theoret. geophys. ; GJI
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  • 96
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    The role of viscous dissipation in the orogenic process (1996)
    In:  Earth planet. Sci. Lett., Warszawa, Zaklad Geofizyki Polskiej Akademii Nauk, vol. 142, no. 1, pp. 271-288, pp. L24313, (ISSN: 1340-4202)
    Details
    Publication Date: 1996
    Keywords: Rheology ; Inelastic ; Geothermics ; Tectonics ; Absorption
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  • 97
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    Interpretation of broad-band seismograms from the Gräfenberg Array: Examples (1983)
    In:  Veröffentlichung des Zentralinstitutes für die Physik der Erde, Jena, Physica-Verlag, vol. 78, no. 1, pp. 2131-2145, pp. L24313, (ISSN: 1340-4202)
    Details
    Publication Date: 1983
    Keywords: Broad-band ; Seismology ; Seismic arrays
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  • 98
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    Thermal and hydraulic aspects of the KTB drill site (1996)
    In:  Geophys. J. Int., New York, Conseil de l'Europe, vol. 124, no. 14, pp. 756-772, pp. B06307, (ISSN: 1340-4202)
    Details
    Publication Date: 1996
    Keywords: Geothermics ; Fluids ; Borehole geophys. ; Modelling ; GJI
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  • 99
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    Comparison of the Alekseev-Mikhailenko method and the reflectivity method (1983)
    In:  Geophys. J. R. astr. Soc., New York, Conseil de l'Europe, vol. 72, no. 1, pp. 541-566, pp. TC2009, (ISSN: 1340-4202)
    Details
    Publication Date: 1983
    Keywords: Synthetic seismograms ; Reflectivity method ; Finite difference method ; Mueller ; Muller ; GJRaS
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  • 100
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    Implications of structural segmentation during earthquakes: the 1995 Egion earthquake, Gulf of Corinth, Greece (1996)
    In:  Journal of Structural Geology, Warszawa, Conseil de l'Europe, vol. 18, no. 12, pp. 1381-1388, pp. L10608, (ISSN: 1340-4202)
    Details
    Publication Date: 1996
    Keywords: Geol. aspects ; Fault zone ; Earthquake ; Structural geology ; JSG
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