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  • 1995-1999  (7,660)
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  • 1995-1999  (7,660)
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  • 1
    Publication Date: 2023-12-05
    Description: Aus zwei Fundhorizonten in Schichten der Unteren Lebacher Gruppe werden im folgenden die Amphibfährte Anthichnium salamandroides und die Reptilfährten Amphisauropus latus, Amphisauropus imminutus, Dromopus lacertoides, Dimetropus leisnerianus, Gilmoreichnus brachydactylus und Gilmoreichnus minimus beschrieben. Hinzu kommen zwei Fährten unsicherer systematischer Stellung: cf. Foliipes abscisus und cf. Hyloidichnus arnhardti. Gemessen an der stratigraphischen Verteilung der Fährten des Thüringer Waldes repräsentiert die Faunenzusammensetzung Oberes Autun.
    Description: Abstract: The amphibian trackway Anthichnium salamandroides and the reptilian trackways Amphisauropus latus, Amphisauropus imminutus, Dromopus lacertoides, Dimetropus leisnerianus, Gilmoreichnus brachydactylus, Gilmoreichnus minimus and in addition to these two trackways of uncertain systematic ränge: cf. Foliipes abscisus and cf. Hyloidichnus arnhardti are described. They have been sampled from two beds within strata of the lower „Lebacher Gruppe". Compared with the Stratigraphie spreading of trackways from the „Thüringer Wald"- area this faunal assemblage represents Upper Autunian.
    Description: 1. Einleitung 2. Fundort und Fundschichten 3. Terminologie 4. Beschreibung der wichtigsten Fährten Anthichnium salamandroides Amphisauropus latus Amphisauropus imminutus Dromopus lacertoides Dimetropus leisnerianus Gilmoreichnus brachydactylus Gilmoreichnus minimus Fährten unsicherer systematischer Stellung 5. Die Faunenelemente und ihr stratigraphischer Aussagewert Schriften
    Description: research
    Keywords: ddc:562 ; Rotliegend ; Tetrapoden ; Saar-Nahe-Becken
    Language: German
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  • 2
    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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  • 3
    Publication Date: 2023-05-12
    Description: Aus dem Schleichsand (Ob. Rupelium) des Mainzer Beckens wird die Art Teredina turnerae n. sp. beschrieben und abgebildet. Der derzeitige Kenntnisstand über Die Gattung Teredina Lamarck, 1818, wird zusammengefaßt und ihre paläogeographische und stratigraphische Verbreitung auf das Paläogen in Europa und Nordamerika eingegrenzt.
    Description: Abstract: A new species of a boring clam from the Schleichsand (U. Rupelium) of the Mainz Basin Teredina turnerae n. sp. is described and figured. The present knowledge of the genus Teredina Lamarck, 1818, is summarized. The paleogeographic and stratigraphic distribution is restricted to the Paleogene in Europe and North America.
    Description: research
    Keywords: ddc:562 ; Mainzer Becken ; Oligozän ; Bivalven
    Language: German
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  • 4
    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
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  • 5
    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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  • 6
    Publication Date: 2022-08-02
    Description: Funde nicht-alpiner Gerölle südlich des altpleistozänen Donaulaufs in der östlichen Iller-Lech-Platte werden als umgelagerte Reste pliozäner Donauschotter gedeutet und geben so erste Hinweise auf ein Ausgreifen der Donau 35-40 km südlich ihres heutigen Laufs. Die bisher als Tertiärrelikt angesehene Dinkelscherbener Altwasserscheide dieses Bereichs kann somit erst im Pleistozän entstanden sein und dürfte kaum am Staufenberg vorbei weiter nach NNO gereicht haben.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 7
    Publication Date: 2022-08-05
    Description: Die MATUYAMA/BRUNHES-Grenze konnte am Mittelrhein in der Schichtenfolge von Kärlich relativ stark eingeengt werden. Sie ist dort älter als die 6. Eiszeit vor heute und liegt in einer Wechselfolge von Sedimenten, die dem „Ville-Interglazial-Komplex" zugeordnet wird. Möglicherweise muß diese Grenze sogar noch etwas tiefer gelegt werden in einen Horizont mit ersten Zeugnissen eiszeitlichen Dauerfrostbodens. In allen anderen untersuchten Lokalitäten ist die Lückenhafbigkeit der Überlieferung zu groß für detailliertere Aussagen. Die MATUYAMA-Epoche ist vorerst sowohl am Rhein wie an der Donau wegen der vorwiegend gröberklastischen Gesteinsfazies nur bedingt mit der Feingliederung des ältesten Pleistozäns korrelierbar. So sind in der Ville (Tgb. Frechen) mehrere altquartäre warmklimatische Tonhorizonte revers magnetisiert (Tonhorizont B2 und C). Darüber folgt ein normal magnetisierter Horizont (Tonhorizont D), der sich ebenfalls noch im Liegenden der Hauptterrassenfolge befindet. Schließlich wurde neuerdings im Liegenden dieser Abfolge ein weiterer, bereits quartärer Horizont (Bl) gefunden, in welchem sich eine Umpolung von normal nach revers vollzieht. Die Schwierigkeit besteht vorerst noch darin, diese Abfolge geobotanisch genauer zu definieren. Die GAUSS-Epoche läßt sich hingegen in einen guten Zusammenhang mit dem mittleren bis höheren Pliozän bringen (Brunssumium bis mittleres Reuverium). Die Tertiär/Quartär-Grenze auf geobotanischer Grundlage kann nach diesen Befunden etwa mit 2 Mio. Jahre vor heute relativ gut festgelegt werden; denn im höchsten Reuverium (C), das zumeist der Erosion zum Opfer gefallen ist, wurde bereits die Umpolung zur reversen Matuyama-Epodie (Beginn rd. 2,4 Mio. Jahre vor heute) gefunden.
    Description: research
    Keywords: ddc:551.7
    Language: German
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  • 8
    Publication Date: 2022-10-06
    Description: Ein Profil im Rotliegenden des Saar-Nahe-Gebietes bei Odernheim/Glan wird beschrieben von der Oberen Lebacher Gruppe (ru) im Liegenden (aufgeschlossen ab Mittl. Lebacher Gruppe) bis zur Grenzlager-Gruppe im Hangenden. Das Spektrum der untersuchten transparenten Schwerminerale umfaßt Zirkon, Turmalin, Granat, Rutil, Apatit und Anatas. Für die Klärung stratigraphischer Fragen erweisen sich transparente Schwerminerale im untersuchten Profil als ungeeignet. Die Einflüsse von Transport, Verwitterung und Diagenese werden kurz diskutiert. Als Muttergesteine kommen teilweise Sedimente, teilweise auch granitoide Gesteine in Frage; als Liefergebiete werden Vogesen und Schwarzwald angesehen.
    Description: Abstract: A profile near Odernheim/Glan through the Lower Permian of the Saar- Nahe area is described. The observed transparent heavy minerals are zircon, tourmaline, garnet, rutile, apatite, and anatase. To clear up stratigraphical questions, heavy minerals are unsuitable in the Odernheim area. Influences of transport, weathering, and diagenesis are discussed briefly. The parent rocks are partly sedimentary, partly granitic rocks; probable regions of provenance are the Vosges Mountains and the Black Forest.
    Description: research
    Keywords: ddc:549
    Language: German
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  • 9
    Publication Date: 2022-09-16
    Description: Die Fauna der Rotliegend-Serien des Saar-Nahe-Gebietes wird in knapper Form mit den wesentlichsten Merkmalen beschrieben. Wegen des Fehlens moderner Bearbeitungen werden einige Gruppen (Bivalven, Insekten) nicht im einzelnen abgehandelt. Verschiedene für das Saar-Nahe-Gebiet neue Formen werden provisorisch beschrieben und bestimmt. Es sind dies: der Ostracod Carbonita sp. H; die Conchostraken Cyzicus (Lioestheria)? sp. W und Cyzicus (Euestheria) sp. P; ein erster Arachnidenrest; der Haifisch Xenacanthus sp. B und ein Elonichthyide; das Reptil Batropetes sp.; die Lebensspuren Planolites? sp., Walpia? sp., Pelecypodichnus sp., Guilielmites sp., Laevicyclus? sp. und verschiedene Arthropodenfährten (Oniscoidichnus sp., Typ N 1 und N 2, Typen LH und LT).
    Description: Abstract: The fauna of the Rotliegendes of the Saar-Nahe area is described in its essential characteristics. Some groups (bivalvs, insects) are not treated in detail because here up-to-date treatments are lacking. Various species formerly unknown from the Saar-Nahe-area are described briefly and are determined provisionaly. These are: the ostracod Carbonita sp. H; the conchostracans Cyzicus (Lioestheria)? sp. W and Cyzicus (Euestheria) sp. P; a first fragment of an arachnid; the shark Xenacanthus sp. B and an elonichthyid palaeoniscid; the reptile Batropetes sp., the trace fossils Planolites? sp., Walpia? sp., Pelecypodichnus sp., Guilielmites sp., Laevicyclus? sp. and various arthropod tracks (Oniscoidichnus sp., type N 1 and N 2, types LH and LT).
    Description: 1. Vorwort. 2. Faunenbeschreibung 2.1. Coelenteraten 2.2. Gastropoden 2.3. Bivalven 2.4. Anneliden 2.5. Crustaceen 2.5.1. Conchostracen 2.5.2. Ostracoden 2.5.3. Malacostracen 2.6. Arachniden 2.7. Insekten und Myriapoden 2.8. Fische 2.8.1. Xenacanthiden 2.8.2. Acanthodier 2.8.3. Dipnoer 2.8.4. Palaeonisciden 2.9. Tetrapoden 2.9.1. Rhachitomen 2.9.2. Lepospondylen 2.9.3. Reptilien 2.10. Lebensspuren. 2.10.1. Freßbauten 2.10.2. Ruhespuren 2.10.3. vermutliche Wohnbauten 2.10.4. vermutliche Weidespuren 2.10.5. Kriech- und Laufspuren Schriften Fossil-Register
    Description: research
    Keywords: ddc:562 ; ddc:567
    Language: German
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  • 10
    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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  • 11
    Publication Date: 2024-03-21
    Description: abstract
    Description: DFG, SUB Göttingen
    Keywords: Rezension
    Language: German
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  • 12
    facet.materialart.
    Unknown
    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-04-01
    Description: Die Wasserhaushalts-Bilanz der Bundesrepublik weist nach KELLER (39) bei einer mittleren Niederschlags-Höhe von 803 mm einen mittleren Abfluß von Boden-Sickerwasser von 320 mm auf. Der durchschnittliche Wasser-Verbrauch von Bevölkerung und Industrie wird mit 58 mm angesetzt. Nach Vorausberechnungen von CLODIUS (11) soll sich der Wasser-Verbrauch bis zum Jahre 2000 verdreifachen. Danach scheint auf den ersten Blick der Grundsatz der Europäischen Wassercharta des Europarates vom 6.5.1968 gegenstandslos: "Die Vorräte an gutem Wasser sind nicht unerschöpflich. Deshalb wird es immer dringender, sie zu erhalten, sparsam damit umzugehen und, wo immer möglich, zu vermehren". Die Diskrepanz besteht darin, daß eine summarische Wasser-Bilanz als Berechnungs-Grundlage nicht ausreicht, weil sie die räumliche und zeitliche Differenzierung des Wasser-Angebotes und -Verbrauchs nicht berücksichtigt. In den Ballungs-Gebieten treten bereits häufig Engpässe in der Wasser-Versorgung auf, die durch eine Zulieferung aus Uberschuß-Gebieten gedeckt werden müssen, wie z.B. die Gegenüberstellungen Ruhrgebiet --- Sauer land; Bremen Harz verdeutlichen. Steigender Wasserverbrauch bedingt gleichzeitig in der Regel auch eine vermehrte Einleitung von Abwasser in das Oberflächen und Grundwasser (WELTE, 77). Folge ist, daß viele Gewässer nicht mehr für die Gewinnung von Trink- oder Brauchwasser in Betracht kommen. Der Versehrnutzungs-Grad unserer Oberflächen-Gewässer hat von 1957 bis 1969 um 50 % zugenommen (81). In vielen Fällen ist es den Wasserwerken kaum noch möglich, Trinkwasser, das den hygienischen Anforderungen nach DIN 2000 (84) entspricht, mit einem ökonomisch vertretbaren Aufwand bereitzustellen (OEHLER, 55).
    Description: research
    Keywords: Physikochemische Bodeneigenschaft ; Bewässerung ; Abwasserverwertung ; Abwasserbeseitigung ; Filtration Zuckerfabrik ; Rieselfeld ; Biologische Abwasserreinigung ; Bewässerung ; Abwasserbeseitigung ; Zuckerfabrik
    Language: German
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  • 13
    facet.materialart.
    Unknown
    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    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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    Selbstverlag Fachbereich Geowissenschaften, FU Berlin
    In:  Herausgeberexemplar
    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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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-04-20
    Description: research
    Keywords: Grundwasserverschmutzung ; Bewässerung ; Abwasser ; Waldbestand
    Language: German
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  • 16
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    In:  Herausgeberexemplar
    Publication Date: 2024-03-06
    Description: Die Pflanzengesellschaften verschiedener feuerländischer Hochmoore wurden nach der Methode von BRAUN-BLANQUET untersucht. Die untersuchten Moore liegen im argentinischen Teil von Feuerland in der Nähe von Ushuaia. Das vorhandene Untersuchungsmaterial läßt zwei neue Hochmoor-Pflanzengesellschaften erkennen: Carici magellanici- phagnetum fimbriati [und] Pernettyo-Sphagnetum. Das Carici magellanici-Sphagnetum fimbriati entspricht dem europäischen Caricetum limosae. Das Pernettyo-Sphagnetum gehört (nur dieses kann bislang gesagt werden) zur Oxycocco-Sphagnetea. Über eine endgültige Zuordnung kann erst entschieden werden, wenn weiteres Untersuchungsmaterial aus den Hochmooren der Südhemisphäre vorliegt. Die chemischen Kennwerte ähneln denjenigen der norddeutschen Hochmoore. Die höheren pH-‚ K-, Ca-‚ Mg- und Na-Werte zeigen die Meeresnähe der feuerländischen Hochmoore an.
    Description: The plant communities of various raised bogs of the Tierra del Fuego were investigated according to the method BRAUN-BLANQUET. The investigated bogs are in the Argentine part of Tierra del Fuego in the vicinity of Ushuaia. The available examination material shows two new bog plant communities: Carici magellanici-Sphagnetum fimbriati [and] Pernettyo-Sphagnetum. The Carici magellanici-Sphagnetum fimbriati corresponds to the European Caricetum limosae. The Pernettyo-Sphagnetum belongs to the Oxycocco-Sphagnetea. Further classification can be decided only after more material from the bogs of the southern hemisphere available for examination. The characteristic chemical values are similar to those of the North-German raised bogs. The higher pH-, K-, Ca-, Mg- and Na-values indicate that the bogs of Tierra del Fuego are close to the ocean.
    Description: Las comunidades vegetales de diferentes turberas sfagnosas de la Tierra del Fuego fueron estudiadas y analizadas de acuerdo con el método BRAUN-BLANQUET. Las zonas pantanosas se encuentran en la parte Argentina de la Tierra del Fuego, cerca de Ushuaia. En virtud del resultado explorativo del material disponible se pueden reconcer dos comunidadas vegetales nuevas en las turberas sfagnosas: e Carici magellanici-Sphagnetum fimbriati [e] Pernettyo–Sphagnetum. El Carici magellanici-Sphagnetum fimbriati corresponde al Caricetum limosae de Europa. El Pernettyo-Sphagnetum pertenece a Oxycocco-Sphagnetea. No se puede decidir sobre una clasificacion mäs detallada hasta que haya mas material exploacion de las turberas sfagnosas del hemisferio sur. Los valores caracteristicos quimicos se parecen a aquellos de las turberas sfagnosas del norte de Alemania. Los contenidos mäs elevados de pH, K, Ca, Mg y Ca demuestran que las turberas sfagnosas de la Tierra del Fuego se encuentran el mar.
    Description: research
    Description: DFG, SUB Göttingen, DGMT
    Keywords: ddc:553.21 ; ddc:581.7 ; Moor ; Torf ; Vegetation ; peatland ; peat
    Language: German
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-04-06
    Description: research
    Keywords: Ausgangsgestein ; Kristallin ; Kristallines Gestein ; Iberische Halbinsel ; Fossiler Boden ; Iberische Halbinsel
    Language: German
    Type: doc-type:book
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  • 18
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-04-06
    Description: research
    Keywords: NIEDERSCHLAG ; BODENBILDUNG ; VENEZUELAS ; ANDENKORDILLERE
    Language: German
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  • 19
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-04-06
    Description: research
    Keywords: STANDORTSFAKTOREN ; OBERHOHE ; FICHTE (PICEA ABIES KARST.) ; HESSEN
    Language: German
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  • 20
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-04-06
    Description: Trotz jahrzehntelanger methodischer Forschung auf dem Gebiet der Bodenfeuchte-Bestimmung sind viele damit zusammenhängende Probleme bislang als technisch nicht gelöst zu betrachten. Wandlungen und Fortschritte im Bereich der boden-hydrologischen und boden-ökologischen Forschung stellen neue Anforderungen an die Meß-Technik. So verlangen z.B. Untersuchungen der Bodenwasser-Bilanz im Felde, die auf der kontinuierlichen Bestimmung hydraulischer Gradienten und der Ermittlung von spezifischen W asser-Leitfähigkelten der einzelnen Boden-Schichten basieren, exakte und kontinuierliche Bestimmungen der Boden-Wassergehalte möglichst dUnnen Boden-Schichten. Dies erweist sich als umso notwendiger, als neuere Untersuchungen zur Saugspannungs-W asser- gehalts-Hysterese bei Wasser-Aufnahme und -Abgabe im Boden gezeigt haben, daß die zur Berechnung erforderlichen Wasser- gehalts-Angaben durch direkte Messungen ermit telt werden sollten und nicht als abgeleitete Größen, z.B. aus der Saugspannung Uber die Wassergehalts- Saugspannungs-Charakteristik, verwendet werden sollten.
    Description: research
    Keywords: Wassergehalt ; Wärmeleitfähigkeit ; Physikochemische Bodeneigenschaft ; Löss ; Lössboden
    Language: German
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  • 21
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    Universität Göttingen,Abteilung Bodenphysik
    In:  Universität Göttingen
    Publication Date: 2024-04-05
    Description: research
    Keywords: Phytotoxizität ; Sorption ; Herbizidbelastung ; Physikochemische Bodeneigenschaft ; Boden-Pflanze-System Kulturboden ; Bodenbiologie ; Einflussgröße ; Herbizid ; Sorption
    Language: German
    Type: doc-type:book
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  • 22
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    In:  Tectonophys., Luxembourg, EGS-Gauthier-Villars, vol. 253, no. 2, pp. 247-270, pp. 2324
    Publication Date: 1996
    Keywords: Fault zone ; Statistical investigations ; Fracture
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  • 23
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    In:  Geophys. J. R. astr. Soc., Luxembourg, EGS-Gauthier-Villars, vol. 46, no. 5652, pp. 575-593, pp. 1310
    Publication Date: 1976
    Keywords: Fault zone ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; GJRaS
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  • 24
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    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
    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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    In:  Geophys. J. R. astr. Soc., Washington D.C., Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 47, no. 6, pp. 301-329, pp. L08305
    Publication Date: 1976
    Keywords: Moment tensor ; SModelling ; Source ; GJRaS
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  • 26
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    In:  Terra Nova, Warszawa, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 8, no. 3, pp. 223-235, pp. 2121
    Publication Date: 1996
    Keywords: Stress ; Physical properties of rocks
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  • 27
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    In:  Phys. Earth Plan. Inter., Beijing, Pergamon, vol. 12, no. 17, pp. 1-50, pp. 2135
    Publication Date: 1976
    Keywords: Tectonics ; Plate tectonics ; Statistical investigations ; Seismicity ; PEPI
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  • 28
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    In:  J. Geophys. Res., San Francisco, Pergamon, vol. 101, no. 20, pp. 8111-8128, pp. 1246
    Publication Date: 1996
    Keywords: Three dimensional ; P-waves ; Shear waves ; Velocity depth profile ; Volcanology ; JGR
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  • 29
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    In:  Bull. Seism. Soc. Am., San Francisco, Pergamon, vol. 86, no. 2, pp. 519-523, pp. 1246
    Publication Date: 1996
    Keywords: Site amplification ; Spectrum ; Error analysis ; BSSA
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  • 30
    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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    In:  J. Geophys. Res., Warszawa, Elsevier, vol. 101, no. 2, pp. 5435-5444, pp. L02307, (ISBN: 0-12-018847-3)
    Publication Date: 1996
    Keywords: Stress ; Statistical investigations ; Data analysis / ~ processing ; Plate tectonics ; JGR
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  • 32
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    In:  Bull. Seism. Soc. Am., Leipzig, Birkhäuser Verlag, vol. 86, no. 6, pp. 66-72, pp. 2366, (ISBN: 0-12-018847-3)
    Publication Date: 1996
    Keywords: Site amplification ; Strong motions ; Finite difference method ; USA ; Waves ; Seismology ; accelerations ; topography ; BSSA
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  • 33
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    In:  Tectonophysics, Luxembourg, Conseil de l'Europe, vol. 264, no. 1-4, pp. 295-308, pp. B04313, (ISBN: 0-12-018847-3)
    Publication Date: 1996
    Keywords: Borehole geophys. ; scientific drilling ; Vertical seismic profiling ; EUROPROBE (Geol. and Geophys. in eastern Europe) ; SG3
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  • 34
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    In:  Journal of Structural Geology, Taipei, Elsevier, vol. 18, no. 11, pp. 1353-1367, pp. TC1002, (ISBN: 0-12-018847-3)
    Publication Date: 1996
    Keywords: paleo ; Stress ; Geol. aspects ; Structural geology ; JSG
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  • 35
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    In:  J. Geophys. Res., Heidelberg, 3-4, vol. 101, no. 11, pp. 25,321-25,336, pp. 1516, (ISBN: 0-12-018847-3)
    Publication Date: 1996
    Keywords: Seismicity ; Friction ; Seismology ; JGR
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  • 36
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    In:  J. Geophys. Res., Heidelberg, North Holland Publishing Company, vol. 101, no. 4, pp. 8595-8604, pp. 1516, (ISBN: 0-12-018847-3)
    Publication Date: 1996
    Keywords: Inelastic ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Earthquake ; JGR
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  • 37
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    In:  Bull. Seism. Soc. Am., Roma, Acad. Roy. des Sciences, vol. 86, no. 1, pp. 477-488, pp. B04102, (ISBN: 0-12-018847-3)
    Publication Date: 1996
    Keywords: Anisotropy ; Local earthquakes ; Borehole geophys. ; USA ; Seismic arrays ; Seismology ; anisotropy ; southern ; California ; BSSA
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  • 38
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    In:  J. Geophys. Res., Bonn, Inst. f. Theoret. Geodäsie, vol. 81, no. 3-5, pp. 3036-3046, pp. B04102, (ISBN: 0-12-018847-3)
    Publication Date: 1976
    Keywords: Modelling ; Seismology ; Least-squares ; Hypocentral depth ; Velocity ; Velocity depth profile ; JGR
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  • 39
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    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)
    Publication Date: 1996
    Keywords: Inversion ; Fracture ; Source
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  • 40
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    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)
    Publication Date: 1996
    Keywords: Fracture ; Source ; Seismology ; JGR
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  • 41
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    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)
    Publication Date: 1996
    Keywords: Modelling ; Boundary Element Method ; Elasticity
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  • 42
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    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)
    Publication Date: 1996
    Keywords: Site amplification ; Modelling ; SH waves ; noksp ; BSSA
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  • 43
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    In:  Tectonophysics, Luxembourg, Pergamon, vol. 257, no. 2-4, pp. 175-188, pp. 2131, (ISBN 1-86239-117-3)
    Publication Date: 1996
    Keywords: Stress ; Geol. aspects ; Physical properties of rocks ; Fracture
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  • 44
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    In:  Geowissenschaften, Amsterdam, Elsevier, vol. 14, no. 7-8, pp. 308-309, pp. 2083, (ISBN 1-86239-117-3)
    Publication Date: 1996
    Keywords: Tectonics ; metamorphic ; China ; scientific drilling ; Geol. aspects
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  • 45
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    In:  J. Geophys. Res., London, Elsevier, vol. 101, no. 8, pp. 27,917-27,942, pp. 2083, (ISBN 1-86239-117-3)
    Publication Date: 1996
    Keywords: Tomography ; Fault zone ; triple ; junction ; Modelling ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; JGR
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  • 46
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    In:  Geophys. J. R. astr. Soc., Luxembourg, U.S. Geological Survey, vol. 44, no. 24, pp. 7-17, pp. B05309, (ISBN 0-471-26610-8)
    Publication Date: 1976
    Keywords: Travel time ; Seismology ; GJRaS ; Dziewonski
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  • 47
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    In:  Tectonophysics, Münster, Amer. Sc., vol. 259, no. 3, pp. 101-116, pp. 1228, (ISBN 0-471-26610-8)
    Publication Date: 1996
    Keywords: Stress ; paleo ; Plate tectonics ; Structural geology ; Sebrier
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  • 48
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    In:  Berichte der Bunsen-Gesellschaft, Münster, Amer. Sc., vol. 80, no. 4, pp. 1059-1081, pp. 1228, (ISBN 0-471-26610-8)
    Publication Date: 1976
    Keywords: Data analysis / ~ processing
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  • 49
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    In:  Geophys. J. Int., Münster, 3, vol. 125, no. 3, pp. 747-767, pp. L11308, (ISBN 0-471-26610-8)
    Publication Date: 1996
    Keywords: AnisotropyS ; Teleseismic events ; GJI
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  • 50
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    In:  Eos, Trans., Am. Geophys. Un., Münster, 3, vol. 77, no. 7, pp. 62, pp. L12311, (ISBN 0-471-26610-8)
    Publication Date: 1996
    Keywords: Earthquake ; China ; AGU
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  • 51
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    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)
    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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  • 52
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    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)
    Publication Date: 1996
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Volcanology ; Stress ; Fracture ; JGR
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  • 53
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    Unknown
    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)
    Publication Date: 1996
    Keywords: Stress ; Tectonics ; Plate tectonics ; intra-plate ; JGR
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  • 54
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    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)
    Publication Date: 1996
    Keywords: Finite difference method ; Three dimensional ; Modelling ; BSSA ; SRICHWALSKI
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  • 55
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    In:  Tectonophys., Bonn, Pergamon, vol. 266, no. 1-4, pp. 33-53, pp. 2144, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1996
    Keywords: Stress ; Finite Element Method ; Modelling ; Borehole geophys. ; Borehole breakouts ; Fault plane solution, focal mechanism ; Golke
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  • 56
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    In:  Tectonophys., Bonn, Pergamon, vol. 266, no. 1-4, pp. 11-24, pp. 2144, (ISBN: 0534351875, 2nd edition)
    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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  • 57
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    In:  Tectonophys., Bonn, Pergamon, vol. 266, no. 1-4, pp. 25-32, pp. 2144, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1996
    Keywords: Stress ; Finite Element Method ; Modelling ; Borehole geophys. ; Borehole breakouts ; Golke
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  • 58
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    In:  Geologisches Jahrbuch Reihe E Geophysik - geophysics, Bonn, Pergamon, vol. 266, no. E7, pp. 3-5, pp. 2144, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1976
    Keywords: Planetology ; moon ; Review article ; geosciences
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  • 59
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    Pergamon
    In:  Physics and Chemistry of the Earth, London, Pergamon, vol. 21, no. 4, pp. 261-265, pp. B05401, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1996
    Keywords: Stress ; Geol. aspects ; Modelling ; cracks and fractures (.NE. fracturing) ; Fault zone ; Plate tectonics ; Strike-slip ; Modelling
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  • 60
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    In:  Tectonophysics, London, Pergamon, vol. 255, no. 3-4, pp. 211, pp. B05401, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1996
    Keywords: paleo ; Stress ; Geol. aspects ; Tectonics ; Plate tectonics
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  • 61
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    In:  J. Geophys. Res., Warszawa, Eötvös Lorand Geophysical Institute of Hungaria, vol. 81, no. 9-12, pp. 3484-3494, pp. 2342, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1976
    Keywords: Velocity ; Laboratory measurements ; cracks and fractures (.NE. fracturing) ; Modelling ; JGR
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  • 62
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    In:  Tectonophysics, Basel, Birkhäuser Verlag, vol. 264, no. 1-4, pp. 191-204, pp. B05S07, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1996
    Keywords: EUROPROBE (Geol. and Geophys. in eastern Europe) ; rifting ; Deep seismic sounding (espec. cont. crust) ; Muller
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  • 63
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    In:  Geophys. J. Int., Luxembourg, Conseil de l'Europe, vol. 127, no. 3-4, pp. 348-362, pp. L17606, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1996
    Keywords: Rheology ; Inelastic ; NOModelling ; Earth rotation ; (The Earth's free) oscillations ; GJI
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  • 64
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    In:  Geophys. J. Int., Luxembourg, Conseil de l'Europe, vol. 127, no. 3, pp. 515-528, pp. L17606, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1996
    Keywords: Moment tensor ; Inversion ; NOModelling ; GJI
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  • 65
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    In:  Earth planet. Sci. Lett., Luxembourg, Conseil de l'Europe, vol. 137, no. 2, pp. 101-108, pp. L17606, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1996
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geol. aspects ; Plate tectonics
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  • 66
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    In:  Geophys. J. R. astr. Soc., Münster, Inst. f. Geophys., Ruhr-Univ. Bochum, vol. 47, no. 1-4, pp. 97-133, pp. B04310, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1976
    Keywords: Source ; Dislocation ; SModelling ; GJRaS
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  • 67
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    In:  Gerl. Beitr. Geophys., Münster, Inst. f. Geophys., Ruhr-Univ. Bochum, vol. 85, no. 5, pp. 415-424, pp. B04310, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1976
    Keywords: Correlation ; Gravimetry, Gravitation ; Geomagnetics ; Data analysis / ~ processing
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  • 68
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    In:  Geophys. Res. Lett., Münster, Inst. f. Geophys., Ruhr-Univ. Bochum, vol. 23, no. 3, pp. 229-232, pp. B04310, (ISBN: 0534351875, 2nd edition)
    Publication Date: 1996
    Keywords: Seismology ; history ; Earthquake ; GRL
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  • 69
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    In:  Engineering Geology, Stuttgart, Conseil de l'Europe, vol. 43, no. 1, pp. 5-9, pp. L17311, (ISSN 0343-5164)
    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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  • 70
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    In:  Tectonophys., Tokyo Univ., Geophys. Inst., Fac. of Science, vol. 266, no. 1-4, pp. 287-300, pp. L23611, (ISSN 0343-5164)
    Publication Date: 1996
    Keywords: Stress ; EUROPROBE (Geol. and Geophys. in eastern Europe) ; Geol. aspects ; paleo
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  • 71
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    In:  Geophys. Prosp., Taipei, Am. Inst. Min. Metal. Petr. Eng., vol. 24, no. 4, pp. 719-724, pp. 2235, (ISSN 0343-5164)
    Publication Date: 1976
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  • 72
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    In:  Geophys. J. Int., Taipei, Am. Inst. Min. Metal. Petr. Eng., vol. 124, no. 2, pp. 105-112, pp. 2324, (ISSN 0343-5164)
    Publication Date: 1996
    Keywords: AnisotropyS ; Physical properties of rocks ; cracks and fractures (.NE. fracturing) ; GJI
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  • 73
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    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)
    Publication Date: 1996
    Keywords: Earthquake ; Japan ; Modelling ; Source ; Seismology ; BSSA
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  • 74
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    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)
    Publication Date: 1996
    Keywords: Rheology ; Creep observations and analysis ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; JGR
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  • 75
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    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)
    Publication Date: 1996
    Keywords: Statistical investigations ; Seismicity ; Earthquake precursor: prediction research ; Data analysis / ~ processing ; cycles
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  • 76
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    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)
    Publication Date: 1996
    Keywords: Seismicity ; Statistical investigations ; JGR
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  • 77
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    In:  Geophys. J. R. astr. Soc., Berlin, Schweizerbart'sche Verlagsbuchhandlung, vol. 47, no. 7, pp. 351-362, pp. 1978, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Publication Date: 1976
    Keywords: MINV ; Velocity analysis ; Layers ; GJRaS
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  • 78
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    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)
    Publication Date: 1996
    Keywords: Non-linear effects ; Anisotropy ; Stress ; Physical properties of rocks ; JGR
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  • 79
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    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)
    Publication Date: 1996
    Keywords: Seismicity ; intraplate ; seismic Moment ; Plate tectonics ; GJI
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  • 80
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    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)
    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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  • 81
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    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)
    Publication Date: 1996
    Keywords: Rheology ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; JGR
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  • 82
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    In:  Phys. Earth Plan. Int., Tokyo, Tokyo University, vol. 11, no. 9, pp. 312-332, pp. 2265, (ISSN 0016-8548, ISBN 3-510-50045-8)
    Publication Date: 1976
    Keywords: Source mechanics ; Plate tectonics ; PEPI
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  • 83
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    In:  Geophys. J. R. astr. Soc., Amsterdam, Univ. Tokyo, vol. 47, no. 1-2, pp. 225-249, pp. 2152, (ISSN: 1340-4202)
    Publication Date: 1976
    Keywords: Love-waves ; Spectrum ; GJRaS
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  • 84
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    In:  J. Geophys. Res., New York, Allerton Press, vol. 81, no. 14, pp. 4885-4896, pp. 2152, (ISSN: 1340-4202)
    Publication Date: 1976
    Keywords: geodyn ; Plate tectonics ; Seismicity ; Subduction zone ; Gravimetry, Gravitation ; JGR
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  • 85
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    In:  Geophys. J. Int., New York, Allerton Press, vol. 124, no. 19, pp. 341-348, pp. L01606, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Shear waves ; Velocity depth profile ; Waves ; Seismics (controlled source seismology) ; Theoret. geophys. ; GJI
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  • 86
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    In:  Earth planet. Sci. Lett., Warszawa, Zaklad Geofizyki Polskiej Akademii Nauk, vol. 142, no. 1, pp. 271-288, pp. L24313, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Rheology ; Inelastic ; Geothermics ; Tectonics ; Absorption
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  • 87
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    In:  Geophys. J. Int., New York, Conseil de l'Europe, vol. 124, no. 14, pp. 756-772, pp. B06307, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Geothermics ; Fluids ; Borehole geophys. ; Modelling ; GJI
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  • 88
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    In:  Phys. Earth Plan. Int., New York, Conseil de l'Europe, vol. 12, no. 5675, pp. 142-150, pp. B07307, (ISSN: 1340-4202)
    Publication Date: 1976
    Keywords: Filter- ; Data analysis / ~ processing ; PEPI
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  • 89
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    In:  Journal of Structural Geology, Warszawa, Conseil de l'Europe, vol. 18, no. 12, pp. 1381-1388, pp. L10608, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Geol. aspects ; Fault zone ; Earthquake ; Structural geology ; JSG
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  • 90
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    In:  Tectonophys., Basel, Elsevier Science Publishers, vol. 253, no. 42, pp. 155-165, pp. L24312, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Moment tensor ; Seismology ; Tectonics ; Fault plane solution, focal mechanism
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  • 91
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    In:  Geophys. J. Int., Basel, Elsevier Science Publishers, vol. 126, no. 1-3, pp. 871-881, pp. 2519, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Plate tectonics ; Earthquake ; Subduction zone ; Strike-slip ; GJI ; LePichon ; Pichon
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  • 92
    facet.materialart.
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    In:  Tectonophysics, Basel, Elsevier Science Publishers, vol. 257, no. 32, pp. 55-70, pp. L03307, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Rheology ; Inelastic ; Hypocentral depth distribution ; Seismicity ; craton ; Geothermics
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  • 93
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    In:  Computers & Geosciences, Tulsa, 450 pp.; 2nd modified and expanded ed., Society of Exploration Geophysics, vol. 22, no. 9, pp. 955-957, pp. B02405, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Pattern recognition ; GIS ; Review article
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  • 94
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    In:  Science, Amsterdam, Conseil de l'Europe, vol. 273, no. 3/4, pp. 1484-1486, pp. B03405, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Earthquake precursor: prediction research ; discussion ; Project report/description
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  • 95
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    In:  Geophys. J. Int., Amsterdam, 4, vol. 124, no. 2, pp. 483-501, pp. 1334, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Surface waves ; Detectors ; Seismology ; red ; silent ; Low frequency ... ; Nabelek ; GJI
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  • 96
    facet.materialart.
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    In:  Bull. Seism. Soc. Am., San Francisco, Pergamon, vol. 86, no. 1-4, pp. 242-254, pp. B05315, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Fore-shocks ; Earthquake hazard ; Subduction zone ; BSSA
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  • 97
    Publication Date: 1996
    Keywords: Site amplification ; Micro-tremor (seismic noise) ; Nakamura ; comparison ; noksp ; BSSA ; SPAROLAI
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  • 98
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    In:  J. Geophys. Res., Stuttgart, Pergamon, vol. 101, no. 41, pp. 803-816, pp. L13613, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Stress ; Fault plane solution, focal mechanism ; Plate tectonics ; Subduction zone ; Earthquake asperities ; JGR
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  • 99
    Publication Date: 1996
    Keywords: Reflectivity ; Vertical seismic profiling ; Borehole geophys. ; Borehole Compensated Sonic log ; Reflection seismics ; Luschen ; Soellner ; Sollner
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  • 100
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    In:  J. Geophys. Res., Kunming, China, 3-4, vol. 101, no. B5, pp. 6179-6191, pp. 2276, (ISSN: 1340-4202)
    Publication Date: 1996
    Keywords: Fault zone ; Earthquake catalog ; paleo ; Seismicity ; Geol. aspects ; JGR ; FROTH ; (Preprint)
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