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  • Other Sources  (25,259)
  • 1995-1999  (25,259)
  • 1999  (9,617)
  • 1998  (7,984)
  • 1996  (7,658)
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  • 1995-1999  (25,259)
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  • 1999  (9,617)
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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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    Ein Grünsandvorkommen im Verzahnungsbereich Meeressand/Rupelton am Südost-Rand des Kreuznacher Rhyolithmassivs bei Fürfeld (Rupelium, Unteroligozän, Mainzer Becken) (1998)
    Details
    Publication Date: 2022-10-21
    Description: Im Westen von Fürfeld wird ein 2,35 m mächtiges Profil mit Grünsanden beschrieben und sedimentpetrographisch sowie paläoökologisch untersucht. Innerhalb des Grünsands ist ein pelitischer Bereich eingeschaltet, in dem eine fossilführende Mergelsteinlage auftritt. Das Profil schließt rupelische Meeressande in Verzahnung mit Peliten auf. Es ist mit dem Grenzbereich Fischschiefer (= Mittlerer Rupelton) zu Oberem Rupelton korrelierbar. Die Küste lag ca. 800 m weiter nördlich. Der pelitische Bereich repräsentiert stabile Küstenbedingungen während einer Stillstandsphase der Rupeltransgression zur Ablagerungszeit des höheren Fischschiefer. Dabei stellten sich in der flachen Fürfelder Bucht dysaerobe Bodenverhältnisse ein, die zu einer eingeschränkten mixotrophen Lucinidenfauna führten. Die Überlagerung durch Grünsand erfolgte durch Sedimentaufarbeitung zu Beginn der Transgression des Oberen Rupelton- Meeres.
    Description: Abstract: In the southwestern part of the Mainz basin near Fürfeld a small outcrop of Palaeogene sediments was exposed during road works. It is situated in the so called Fürfeld bay and contains an alternation of greensand with pelitic sediment. Within the pelitic sediment an intercalated marlstone layer bears bivalves and fish remains. The sequence represents the transition between the marine coastal sand and the basin clay of the Rupelian. The Fischschiefer = M.Rupelton)/Upper Rupelton boundary is situated within the section. At depositional time the coast was sitvated 800 m to the north. The pelitic sediment is formed under stable coastal environment during sedimentation ofthe late Fischschiefer. Dysaerobic soupground led to a mixotrophic lucinid shell fauna. The overlaying greensand represents reworking of sediment during the beginning of the Upper Rupelton transgression.
    Description: research
    Keywords: ddc:551.304 ; ddc:562
    Language: German
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  • 3
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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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  • 4
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    Hydrogeologische und hydrochemische Besonderheiten der Grundwässer im Mündungsbereich der Ahr (1998)
    Details
    Publication Date: 2022-10-26
    Description: Die Niederterrassenaquifere der „Goldenen Meile” und des Unteren Ahrtales zwischen Bad Breisig, Sinzig und Bad Neuenahr stellen ergiebige Porengrundwasserleiter dar. Mehrere unterschiedliche Grundwassertypen sind verbreitet. Die physiko-chemischen Eigenschaften der Grundwässer unterscheiden sich im südlichen Bereich der Goldenen Meile deutlich von denjenigen im nördlichen Teil des Untersuchungsgebietes. Die Grundwasserhydraulik wird maßgeblich durch den ergiebigen ahrbegleitenden West-Ost gerichteten Grundwasserstrom aus dem Ahrtal bestimmt. Die Grundwässer des Unteren Ahrtales sind durch Mineralwasserzutritte verändert.
    Description: Abstract: The aquifers of the „Goldene Meile” and of the Lower Ahr between Bad Breisig, Sinzig and Bad Neuenahr abound in water. Several types of groundwater are found. The physical and chemical qualities of ground waters differ between south and north part of the investigated area. The hydraulic system is dominated by the groundwaters of der Ahr Valley. The chemical differences are caused by ascent of acid mineralwaters, in the Ahr Valley. In the south part of the „Goldene Meile” there is no recognizable change of ground water quality caused by acid mineral water.
    Description: 1. Einleitung . 2. Geologisch-geographische Übersicht 3. Hydrogeologie 3.1. Grundwasserhydraulik 3.2. Hydrochemische Beschaffenheit der Grundwässer 3.2.1. Grundwässer der „Goldenen Meile“ 3.2.2. Grundwässer der Ahrniederterrasse 3.2.3. Grundwässer der Ost-Eifel 3.2.4. Tiefenwässer 3.2.5. Mischwässer der Niederterrasse 4. Schlussfolgerungen Schriften
    Description: research
    Keywords: ddc:553.79
    Language: German
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  • 5
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    Die Typuslokalität „Hohenrheiner Hütte”: Emsquarzit, Hohenrhein- oder Laubach-Schichten? (1998)
    Details
    Publication Date: 2022-10-18
    Description: An der unteren Lahn sind bei Lahnstein/Hohenrhein (TK25 Blatt 5611 Koblenz) die klastischen Serien des Ober-Ems aufgeschlossen. Wegen der regelmäßigen Fehlinterpretation von Stratigraphie und Tektonik der hier anstehenden Schichtenfolge wurden die regionalen Verhältnisse genauer untersucht und dargestellt. Die Aufnahmen beschreiben das oberhalb der Bundesstraße 260 (Bäderstraße) aufgeschlossene Profil zwischen Lichter Kopf und Mehrsberg, insbesondere zur Klärung von geographischer Position, Raumlage und Abgrenzung der klassischen Typuslokalität der Hohenrhein- Schichten oberhalb der ehemaligen Hohenrheiner Hütte im Bereich der Ruppertsklamm. Nach biostratigraphischen und lithologisch-faziellen Unterscheidungskriterien ist die Typlokalität der Hohenrhein-Schichten sensu Maurer (1882), die FoLLmann (1925) unter Einbeziehung der ‚Plattensandsteine mit Homanolotus scabrosus” neu fasste, im Bereich nordwestlich der Ruppertklamm zu suchen. Dieser Abschnitt gehört hier — ebenso wie die im Hangenden, südöstlich der Ruppertsklamm folgenden Laubach Schichten — zur steil lagernden Süd-Flanke einer Südost-vergenten Sattelstruktur (Niederlahnsteiner Sattel), in deren Kernbereich und flach lagernder Nordwest-Flanke der Emsquarzit zu Tage tritt. In der südöstlichen Fortsetzung leitet ein tektonisch komplex gebauter Abschnitt normallagernder Oberems-Schichten in die weit gespannte, schwach Nordwest- vergente Sattelstruktur des Mehrsberges über (Oberlahnsteiner Sattel). Im Sattelkern stehen hier noch die Serien des höchsten Unter-Ems (obere Nellenköpfchen- Schichten) an, die an den Flanken von den sandig-quarzitischen Abfolgen des Emsquarzits begleitet werden. Die Oberems-Schichten von Mehrsberg und Lichter-Kopf gehören damit zu verschiedenen, durch komplizierten Schuppenbau getrennten Zügen und können entsprechend nicht — wie häufig vermutet wurde — in einer geschlossenen, stratigraphischen Abfolge betrachtet werden.
    Description: Abstract: Near the confluence of the rivers Lahn into the Rhine southeast of Koblenz, the strata of the Lower Devonian succession are well exposed in many outcrops and quarries. A location named „Hohenrheiner Hütte” near the gorge of Ruppertsklamm is mentioned as locus typicus of the „Hohenrhein-Schichten“ sensu Maurer (1882) of Upper Emsian age. Due to an unfortunate description of this location by FoLLmann (1925), a quarry in which the Laubach-Schichten are actually exposed, but are designated as Hohenrhein-Schichten. Kocn (1880) also describes distinctive Emsquarzit at the same location. Thus, three different strata of the Upper Emsian are given the same location „Hohenrheiner Hütte“. Field investigations were made for the construction of a cross-section showing the structural setting of the strata, and to assure their correct stratigraphical classification, a distinction by fossils and lithofacies was made. The resulting locus typicus of the Hohenrhein-Schichten is on the northwest side of the Ruppertsklamm, that of the Laubach- Schichten is found southeastwards of the Hohenrhein-Schichten directly at the road to Bad Ems. These two outcrops are set on the southeastern flank of the southeastvergent Niederlahnstein-Anticline where the Emsquarzit is also exposed. More southeastwards faults seperate the Niederlahnstein-Anticline from the overthrusted Oberlahnstein-Emsquarzit-Anticline, where even youngest Lower Emsian (Nellenköpfchen- Schichten) can be found. The Oberlahnstein-Anticline separates the flank from the core of the Mosel-Syncline.
    Description: research
    Keywords: ddc:554.3
    Language: German
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  • 6
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    Der Meeressand (Rupelium, Oligozän) der Sandgrube „Faber“ bei Siefersheim in Rheinhessen (Mainzer Becken) (1999)
    Details
    Publication Date: 2022-09-29
    Description: In einer Sandgrube bei Siefersheim wird ein 7,2 m mächtiges, durchgehend fossilführendes Profil im oligozänen Meeressand beschrieben. Es enthält eine diverse Fauna und lässt sich mit Hilfe von Foraminiferen biostratigraphisch mit anderen Meeressandprofilen und dem Mittleren Rupelton (Fischschiefer) korrelieren. Aufgrund der Sedimentologie, Mikrofazies und Karbonatzementstratigraphie sowie der Fossilführung des Profils kann eine Genese der Sande im Subtidal- bis Intertidalbereich an einem steilen Kies- bis Sandstrand nachgewiesen werden. So treten in den liegenden, kiesigen Partien des Profils vadose Zementtypen auf, die typisch für Beachrock sind. Die Fossilführung und die damit durchgeführten Paleocommunityanalysen zeigen eine transgressive Entwicklung mit allmählicher Wassertiefenzunahme innerhalb einer teilweise geschützten Bucht im Einflussbereich einer nahen Klippe.
    Description: Abstract: A 7.2 m thick fossiliferous section of oligocene coastal sands was examined in a sand pit near Siefersheim (Mainz Basin, Germany). The sedimentology, the microfacies, the fabrics of carbonate cements and the fossil record suggest a sedimentation on a steep sub- to intertidal gravel- or sandbeach. So on the one hand vadose Mg-calcitic beachrock cements (submicrocrystalline cement and meniscus cement) occur only in the underlying rhyolite-gravel beds. On the other hand cemented bioclast sands of the capping sand layers show early diagenetic recrystallized fibrous cements and the top rhyolite-rubble and breccia beds contain late diagenetic Fe-calcitic drusy mosaic cements. For palaeocommunity-analysis the fossil record was applied. As a result five invertebrate- palaeocommunities with high contents of sessil suspension feeders and moderate diversities could be identified. They show an increase in water depth from about 0 to 25 m from the basal layer to the top, corresponding with a sea level rise of about 35 m. Summing up, it may be said that the sediments examined represent a gradual transgressive development in a partly protected bay in the neighbourhood of a rhyolithic cliff. The biostratigraphical correlation of the Siefersheim section with other Mainz Basin coastal sand profiles and the basin facies of the Middle Rupelian clay (the so called fish shale) was conducted on the basis of foraminifers.
    Description: research
    Keywords: ddc:562 ; ddc:551.304
    Language: German
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  • 7
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    Molluskenzonierung in den Cerithienschichten des Mainzer Beckens (1998)
    Details
    Publication Date: 2022-09-29
    Description: Die lokale aquatische Molluskenzonierung der Cerithienschichten (Oberoligozän) wird modifiziert durch Einfügung einer Subzone Vc, die durch das Erscheinen von Mancosinodia manca definiert ist. Dieser Bivalve erscheint eher als Isognomon spp., dessen gesamte Reichweite in den Cerithienschichten die nachfolgende Zone VI definiert.
    Description: Abstract: The local aquatic mollusk zonation of the Cerithienschichten Formation (Late Oligocene) ofthe Mainz Basin is emended by the insertion of a subzone Vc, which is defined by the first appearance of Mancosinodia manca (Braun). This bivalve was previously thought to appear simultaneously with Isognomon spp. the total range of which defines the subsequent zone VI.
    Description: research
    Keywords: ddc:562
    Language: German
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  • 8
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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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  • 9
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    Neue Fossilfunde aus dem Unterdevon an Rhein und Mosel (Geologische Kartevon Rheinland-Pfalz, Blatt 5611 Koblenz), Teil 1: Unterems (1999)
    Details
    Publication Date: 2022-11-30
    Description: Neue Fossilfunde vorwiegend aus dem hohen Unterems der Rittersturzund Nellenköpfchen-Schichten werden beschrieben. Die unterschiedliche Zusammensetzung der Fauna in Schilien und Schieferfolgen wird diskutiert. Es wird vermutet, dass die unruhigen Sedimentationsverhältnisse im Wattbereich des Nellenköpfchens bei Koblenz, verbunden mit einem besonders häufigen Wechsel von Erosion und Sedimentation, Brachiopoden gegenüber den Bivalvia benachteiligten.
    Description: Abstract: Biostratigraphic fossil research in the Koblenz-area (Lower Devonian, Lower Emsian, Rhenish Massiv) summarizes rieh Bivalvia faunas mainly from the upper part of the Vallendar substage. The „Nellenköpfchen-Schichten" present tidal environment with changing sedimentary conditions. Muddy Sediments occasionally contain numerous Bivalvia, homalonotid trilobites and burrows of homalonotids. The fossil record of the massive sandstones is dominated by shell-beds (induced by hurricanes) containing mainly broken valves of non-autochthonous Bivalvia and brachiopods. Well preserved Palaeoneilo Maureri (Bivalvia) possibly show nearly allochthonous living conditions. In contrast to the tidal embedding of the Nellenköpfchen locality the increment of normal marine Sedimentation with brachiopod dominated shell-beds (Chonetinae) can be observed between Koblenz-Moselweiß and Koblenz-Lay.
    Description: research
    Keywords: ddc:562 ; Rheinisches Schiefergebirge ; TK 5611 ; Unterdevon ; Brachiopoden ; Trilobiten ; Bivalven
    Language: German
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  • 10
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    Paläontologische und geologische Bemerkungen über die Hohenrhein- Schichten (Rheinisches Schiefergebirge, Ober-Ems) an der Typuslokalität im unteren Lahntal (1998)
    Details
    Publication Date: 2023-06-09
    Description: Die geographische Raumlage der Typuslokalität der Hohenrhein- Schichten (Rheinisches Schiefergebirge, Unterdevon, Ober-Ems) wird mit Hilfe von litho- und biostratigraphischen Kriterien festgelegt. Neue Ergebnisse über die Sedimentologie der Schichten und die Taphonomie der darin enthaltenen Fossilien werden vorgestellt.
    Description: Abstract: The geographical location of the type locality of the Hohenrhein-beds (Rheinisches Schiefergebirge, Lower Devonian, Upper Emsian) has been established with the aid of litho- and biostrafigraphical criteria. New results on sedimentology of the strata and faphonomy of the fossils in the Hohenrhein-beds is presented.
    Description: research
    Keywords: ddc:562 ; Rheinisches Schiefergebirge ; Lahntal ; TK 5611 ; Unterdevon ; Stratigraphie ; Brachiopoden
    Language: German
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  • 11
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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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  • 12
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    Torf als nachwachsender Rohstoff (1999)
    In:  Herausgeberexemplar
    Details
    Publication Date: 2024-02-27
    Description: Schwach zersetzter Sphagnum-Torf (Weißtorf) ist ein wertvoller Rohstoff, der für eine Reihe spezieller Anwendungen, insbesondere im Erwerbsgartenbau, schwer substituierbar ist. In West- und Mitteleuropa ist bereits ein Großteil der Vorräte aufgebraucht und wird zunehmend Weißtorf aus Nord- und Ost-Europa sowie Kanada importiert. Langfristig werden die Weißtorf-Vorräte und wachsende Hochmoore nur in Reservaten und in kommerziell nicht erschließbaren Regionen überdauern. Es ist daher an der Zeit, in eine Phase der nachhaltigen Nutzung von Torfen, die Paludikultur, einzutreten. Daß eine Rotationskultur junger Sphagnum-Torfe technisch machbar ist, zeigen Erfahrungen mit dem Sphagnum-Harvesting sowie mit der Revitalisierung von Hochmooren zu Naturschutzzwecken. Die Paludikultur wirft Fragen auf zur Auswahl geeigneter Sphagnum-Sippen, zu Techniken der Etablierung und Beerntung von Moorflächen, zur Optimierung der Erträge und Substratqualitäten, zu erforderlichen Flächengrößen, zur Rentabilität und zu möglichen positiven oder negativen Nebenwirkungen. Diese Aspekte werden ansatzweise diskutiert. In Mitteleuropa stellen insbesondere abgetorfte Hochmoore und andere Bergbaufolgelandschaften ein Flächenpotential für die Paludikultur dar.
    Description: Slightly humified Sphagnum peat is a valuable resource that is difficult to be substituted in professional horticulture. In West- and Central Europe, the stocks are nearly exhausted and peat is increasingly imported. At the long run, Sphagnum moss peat and virgin Sphagnum bogs may only survive in nature reserves or in areas that are technically and commercially inaccessible. Time has, therefore, come for peat extraction to develop into sustainable peat cultivation: paludiculture. Experiences with Sphagnum-harvesting and restoration of cut-over bogs indicate that a rotation culture of young Sphagnum peat is technically possible. A future paludiculture implies the identification of optimal conditions and Sphagnum taxa for peat accumulation, the development of adequate cultivation and retrieval techniques, an estimation of necessary areas and economics, and an assessment of possible positive and negative side effects. This paper presents a review of these aspects. Suitable areas for paludiculture in Central-Europe may include cut-over bogs and other exhausted open-cast mining areas.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:553.21 ; ddc:630 ; Moor ; Torf ; Sphagnum ; Substrat ; Paludikultur ; peatland ; peat
    Language: German
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  • 13
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    A combined structural interpretation based on seismic data and 3-D gravity modeling in the northern Puna/Eastern Cordillera, Argentina (1998)
    Selbstverlag Fachbereich Geowissenschaften Freie Universität Berlin
    In:  SUB Göttingen | 98 B 4059
    Details
    Publication Date: 2024-02-14
    Description: Die Andenkordillere entstand entlang des westlichen Randes von Südamerika aufgrund der Subduktion der ozeanischen Nazca-Platte unter die kontinentale Südamerikaplatte seit dem Jura. Als solche werden die Anden als ein klassisches Beispiel eines Orogens entlang eines aktiven Kontinentalrandes betrachtet. Obwohl die gegenwärtige Physiographie das Ergebnis der Andinen Tektonik ist, sind die Zentralanden das Ergebnis von einem komplexen Zusammenspiel von Präkambrischen und Paläozoischen Terrane-Akretionen und Phasen von Kompression und Extension. Die Puna und die Ostkordillere spielen in diesem Zusammenhang eine entscheidende Rolle in der tektonischen Entwicklung der Zentralanden. Die vorliegende Untersuchung befasst sich mit dem Gebiet der nördlichen argentinischen Puna und der Ostkordillere, von etwa 22°S bis 24°S und 65 °W bis 66°30' W. Es wurden etwa 1200 km Seismik interpretiert, deren Ergebnis als Randbedingung in die Konstruktion des gravimetrischen 3D Modells des Gebietes einging.
    Description: The Andes Mountains developed along the western margin of SouthAmerica in response to the subduction of the oceanic Nazca Plate below the South American plate since the Jurassic times. It is considered as one of the classic examples of a mountain chain developed in an active continental margin. Although their present physiography is given by the Andean tectonics, the Central Andes are the result of complex interplay of Precambrian and Paleozoic terrane accretion and phases of compression and extension. The Puna and Eastern Cordillera represent key elements in the tectonic evolution of the Central Andes. The present study covers a region of the northern Puna and Eastern Cordillera extending from approximately 22°S to 24°S and 65 °W to 66°30'W in Argentina. About 1200 km of seismic lines were interpreted and were used as a geometrical constraint for the construction of a 3D gravity model of the area.
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:558 ; Anden ; Argentinien ; Seismik
    Language: English
    Type: doc-type:book
    Format: 192
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  • 14
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    JÜRGEN SCHWAAR − Träger der C.A. WEBER - Medaille (1999)
    In:  Herausgeberexemplar
    Details
    Publication Date: 2024-03-21
    Description: Laudatio anlässlich der Verleihung der C. A. WEBER-Medaille an Jürgen Schwaar während der 16. Jahreshauptversammlung der DGMT am 23. Juni 1999 in Schleswig.
    Description: editorial
    Description: DFG, SUB Göttingen
    Keywords: Laudatio
    Language: German
    Type: doc-type:article
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  • 15
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    Moore auf der Alaska Peninsula — Ergebnisse vegetationskundlicher Untersuchungen — (1999)
    In:  Herausgeberexemplar
    Details
    Publication Date: 2024-03-21
    Description: Alaska weist eine Vielzahl von Feuchtgebieten und Pfianzengesellschaften auf. Besonders moorreich ist die Alaska Peninsula. Dort wurde ein Moorkomplex (muskeg) in unmittelbarer Nähe der Mt. Peulic Lodge (Ugashik-Seen) anhand von vegetationskundlichen Aufnahmen untersucht. Im untersuchten Moorkomplex dominierten Zwergsträucher, Seggenarten und Moose. Insgesamt konnten 9 verschiedene Vegetationstypen aufgrund von Oberfiächenstrukturen und Vegetation unterschieden werden: deckenmoorartige Strukturen, Bultkuppen, seitliche Bultränder, Schlenken, Wildwechsel, zwei verschiedene teppichartige Matten, rasenartige Horizonte und Wasserlachen.
    Description: Alaska carries a great variety of wetland plant communities, above all the Alaska Peninsula is very rich in mires. One of these mire complexes (muskeg) in the vicinity of the Mt. Peulic Lodge (Lake Ugashik) was investigated by vegetation studies and documented by phytosociological relevés according to the principles of the BRAUN-BLANQUET-school. The mire vegetation was dominated by dwarf shrubs, sedges, and mosses. 9 different vegetation types were ascertained on the basis of topography and floristical composition. These were blanket bog-like structures, elavated hummocks, lateral sites of hummocks, interspersed runnels and hollows, game pathes, two different types of flat mosscarpets, lawn-like vegetation structures, and plant associations of small pools.
    Description: research
    Description: DFG, SUB Göttingen
    Keywords: ddc:581.7 ; Moor ; Vegetation ; peatland
    Language: German
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  • 16
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    Hinweise auf Bücher zum Thema „Moor und Torf” (1996)
    In:  Herausgeberexemplar
    Details
    Publication Date: 2024-03-21
    Description: abstract
    Description: DFG, SUB Göttingen
    Keywords: Rezension
    Language: German
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  • 17
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    Beiträge zur Wirbeltier-Paläontologie (1998)
    Selbstverl. Fachbereich Geowissenschaften, FU Berlin, Berlin
    In:  Herausgeberexemplar
    Details
    Publication Date: 2024-04-17
    Description: Gerhard Hahn & Renate Hahn: Neue Beobachtungen an Plagiaulacoidea (Multituberculata) des Ober-Juras 1 . Zum Zahn-Wechsel bei Kielanodon. ... 1 ; Gerhard Hahn & Renate Hahn: Neue Beobachtungen an Plagiaulacoidea (Multituberculata) des Ober-Juras 2. Zum Bau des Unterkiefers und des Gebisses bei Meketibolodon und bei Guimarotodon. ... 9 ; Gerhard Hahn & Renate Hahn: Neue Beobachtungen an Plagiaulacoidea (Multituberculata) des Ober-Juras 3. Der Bau der Molaren bei den Paulchoffatiidae. ... 39 ; Gerhard Hahn & Renate Hahn: Neue Beobachtungen an Plagiaulacoidea (Multituberculata) des Ober-Juras 4. Ein Vertreter der Albion baataridae im Lusitanien Portugals. … 85 ; Bernard Krebs: Drescheratherium acutum gen. et sp. nov., ein neuer Eupanthotherier (Mammalia) aus dem Oberen Jura von Portugal. ... 91 ; Rolf Kohring: Neue Schildkröten-Eischalen aus dem Oberjura der Grube Guimarota (Portugal). ... 113 ; Thomas Martin: The premolars of Crusafontia cuencana (Dryolestidae, Mammalia) from the Early Cretaceous (Barremian) of Spain. ... 119 ; Spyridon M. Bellas, Karina Kussius, Julia K. Kommerell & Jürgen Kriwet: Integrated biostratigraphical approach of the Neogene Pigadia basin of Karpathos Island (Dodecanes Group, Greece) - Implications on the depositional palaeoenvironment based on calcareous nannofossils, ostracodes and facies development data with special references to Messinian fish assemblages. ... 129 ;
    Description: thesis
    Description: DFG, SUB Göttingen
    Keywords: ddc:560 ; Paläontologie
    Language: German , English
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  • 18
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    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
    Type: doc-type:book
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  • 19
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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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  • 20
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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
    Details
    Publication Date: 1996
    Keywords: Fault zone ; Statistical investigations ; Fracture
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  • 21
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    Development of fault discontinuities in shear experiments (1998)
    In:  Tectonophysics, Luxembourg, EGS-Gauthier-Villars, vol. 293, no. 1-2, pp. 45-59, pp. 2324
    Details
    Publication Date: 1998
    Keywords: Laboratory measurements ; Fault zone ; Fracture ; Rock mechanics
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  • 22
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    Methodology for using precarious rocks in Nevada to test seismic hazard models (1999)
    In:  Bulletin of the Seismological Society of America, Luxembourg, EGS-Gauthier-Villars, vol. 89, no. 2, pp. 456-467, pp. 1310
    Details
    Publication Date: 1999
    Keywords: Nuclear explosion ; Earthquake hazard ; Seismology ; BSSA
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    BIBLIOGRAPHY SEISMOLOGY
  • 23
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    Local stress fields and intraplate deformation of Iberia: variations in spatial and temporal interplay of regional stress sources (1999)
    In:  Tectonophysics, Luxembourg, EGS-Gauthier-Villars, vol. 305, no. 1-3, pp. 153-164, pp. L23608
    Details
    Publication Date: 1999
    Keywords: Stress ; Tectonics ; Geol. aspects ; Munoz
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  • 24
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    Further seismic properties of a spring-block earthquake model (1999)
    In:  Geophys. J. Int., Luxembourg, EGS-Gauthier-Villars, vol. 139, no. 2, pp. 410-418, pp. L23303
    Details
    Publication Date: 1999
    Keywords: Modelling ; Statistical investigations ; SOC ; Seismicity ; GJI
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  • 25
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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
    Details
    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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  • 26
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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
    Details
    Publication Date: 1996
    Keywords: Stress ; Physical properties of rocks
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  • 27
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    A model for induced seismicity caused by hydrocarbon production in the western Canada sedimentary basin (1999)
    In:  Canad. J. Earth Sci., Warszawa, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 36, no. 1, pp. 47-64, pp. 2121
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    Publication Date: 1999
    Keywords: Induced seismicity ; Modelling ; Source ; Stress
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  • 28
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    The 17 August 1999 Izmit earthquake (1999)
    In:  Science, Hannover, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 285, no. 5435, pp. 1858-1859, pp. L03607
    Details
    Publication Date: 1999
    Keywords: Earthquake ; NAF ; Turkey ; Source parameters ; Geol. aspects
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  • 29
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    Results from geodetic measurements in the western part of the African-Eurasian plate boundary (1999)
    In:  Tectonophys., Ottawa, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 294, no. 3-4, pp. 261-269, pp. L14310
    Details
    Publication Date: 1999
    Keywords: Geodesy ; Plate tectonics ; Crustal deformation (cf. Earthquake precursor: deformation or strain)
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  • 30
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    Crustal deformation during 1994--1998 due to oblique continental collision in the central Southern Alps, New Zealand, and implications for seismic potential of the Alpine fault (1999)
    In:  J. Geophys. Res., Leiden, Noordhoff, vol. 104, no. B11, pp. 25,233-25,255, pp. 1892
    Details
    Publication Date: 1999
    Keywords: Plate tectonics ; Global Positioning System ; Earthquake hazard ; Seismicity ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Subduction zone ; Modelling ; 1206 ; Geodesy ; Crustal ; JGR ; movements--interplate ; (8155) ; 1243 ; Space ; geodetic ; surveys ; 8102 ; Tectonophysics ; Continental ; contractional ; orogenic ; belts ; 8150 ; Plate ; boundary--general ; (3040)
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  • 31
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    Redistribution of dynamic stress during coseismic ruptures: Evidence for fault interaction and earthquake triggering (1999)
    In:  Journal of Geophysical Research, Beijing, Pergamon, vol. 104, no. B7, pp. 14925-14945, pp. B02211
    Details
    Publication Date: 1999
    Keywords: Stress ; Stress drop ; Fault zone ; JGR
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  • 32
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    Multi-wavelet analysis of three-component seismic arrays: application to measure effective anisotropy at Pinon Flats, California (1999)
    In:  Bull. Seism. Soc. Am., Ottawa, Bundesanstalt für Geowissenschaften und Rohstoffe, vol. 89, no. 3, pp. 693-705, pp. 2371
    Details
    Publication Date: 1999
    Keywords: Seismology ; Data analysis / ~ processing ; Three component data ; Anisotropy ; Wavelet processing ; BSSA
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  • 33
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    Dynamics of sediment subduction-accretion at convergent margins: Short-term modes, long-term deformation, and tectonic implications (1999)
    In:  Journal of Geophysical Research, Leiden, Noordhoff, vol. 104, no. B8, pp. 17573-17601, pp. 2371
    Details
    Publication Date: 1999
    Keywords: Subduction zone ; Plate tectonics ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Geol. aspects ; Friction ; bending ; flexure ; GeodesyY ; Finite Element Method ; Modelling ; sandbox ; analog ; incompressible ; noncohesive ; Coulomb ; flow ; JGR
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  • 34
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    In situ stress data from the Jura Mountains - new results and interpretation (1999)
    In:  Terra Nova, Luxembourg, Conseil de l'Europe, vol. 11, no. 1, pp. 9-15, pp. 1892
    Details
    Publication Date: 1999
    Keywords: Stress ; Tectonics
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  • 35
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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
    Details
    Publication Date: 1996
    Keywords: Three dimensional ; P-waves ; Shear waves ; Velocity depth profile ; Volcanology ; JGR
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  • 36
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    Properties and implications of dynamic rupture along a material interface (1998)
    In:  Bull. Seism. Soc. of America, Beijing, Pergamon, vol. 88, no. 4, pp. 1085-1094, pp. 2135
    Details
    Publication Date: 1998
    Keywords: Fracture ; Friction ; Source ; Rock mechanics ; Dynamic ; BSSA
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  • 37
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    Properties of seismic fault zone waves and their utility for imaging low-velocity structures (1998)
    In:  J. Geophys. Res., Beijing, Pergamon, vol. 103, no. B8, pp. 12,567-12,585, pp. 2135
    Details
    Publication Date: 1998
    Keywords: Waves ; Channel waves ; Low velocity layer ; Seismology ; Fault zone ; JGR ; 5100 ; Physical ; properties ; of ; rocks ; 7260 ; Seismology ; Theory ; and ; modeling ; 8123 ; Tectonophysics ; Dynamics, ; seismotectonics ; 8010 ; Structural ; geology ; (8165) ; Fractures ; and ; faults
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  • 38
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    Self-driven mode switching of earthquake activity on a fault system (1999)
    In:  Earth planet. Sci. Lett., Beijing, Pergamon, vol. 172, no. 1-2, pp. 11-21, pp. 2135
    Details
    Publication Date: 1999
    Keywords: Fault zone ; Seismicity ; Friction ; EPSL
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  • 39
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    Generic finite-fault model for ground-motion prediction in eastern North America (1999)
    In:  Bull. Seism. Soc. Am., San Francisco, Pergamon, vol. 89, no. 3, pp. 608-625, pp. 1246
    Details
    Publication Date: 1999
    Keywords: Seismology ; Modelling ; Strong motions ; Earthquake hazard ; Earthquake risk ; BSSA
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  • 40
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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
    Details
    Publication Date: 1996
    Keywords: Site amplification ; Spectrum ; Error analysis ; BSSA
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  • 41
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    Comment: United Nations encourages sharing of information on disaster forecasting technologies (1999)
    In:  Eos, Trans., Am. Geophys. Un., Paris, Pergamon, vol. 80, no. 20, pp. 231, pp. 1246
    Details
    Publication Date: 1999
    Keywords: Earthquake hazard ; Earthquake risk ; Earthquake precursor: prediction research ; policy
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  • 42
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    The Somma-Vesuvius stress field induced by regional tectonics: evidences from seismological and mesostructural data (1998)
    In:  J. Volcanology and Geothermal Research, Warszawa, ITA & AITES & Pergamon, vol. 82, no. 22, pp. 199-218, pp. L21303
    Details
    Publication Date: 1998
    Keywords: Volcanology ; Stress ; Deep seismic sounding (espec. cont. crust) ; Tectonics
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  • 43
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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)
    Details
    Publication Date: 1996
    Keywords: Geodesy ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; post-glacial ; uplift ; Project report/description
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  • 44
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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)
    Details
    Publication Date: 1996
    Keywords: Stress ; Statistical investigations ; Data analysis / ~ processing ; Plate tectonics ; JGR
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  • 45
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    Thin-plate and thin-shell finite element programs for forward dynamic modeling of plate deformation and faulting (1999)
    In:  Computers and Geosciences, Warszawa, Elsevier, vol. 25, no. 4, pp. 383-394, pp. L02307, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Finite Element Method ; Modelling ; Plate tectonics ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; C&G
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  • 46
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    Global finite-element model makes a small contribution to intraplate seismic hazard estimation (1999)
    In:  Bull. Seism. Soc. Am., Warszawa, Elsevier, vol. 89, no. 6, pp. 1642-1647, pp. L02307, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Seismology ; Earthquake hazard ; Finite Element Method ; Stress ; Modelling ; BSSA
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  • 47
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    The importance of overpressure timing and permeability evolution in fine-grained sediments undergoing shear (1998)
    In:  Journal of Structural Geology, Taipei, Elsevier, vol. 20, no. 8, pp. 1013-1022, pp. 2091, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1998
    Keywords: Physical properties of rocks ; Fluids ; Stress ; Rock mechanics ; Structural geology ; JSG
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  • 48
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    Models of ground deformation from vertical volcanic conduits with application to eruptions of Mount St. Helens and Mount Etna (1999)
    In:  Journal of Geophysical Research, Taipei, Elsevier, vol. 104, no. B5, pp. 10,531-10,542, pp. 2091, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Modelling ; Volcanology ; Italy ; USA ; JGR
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  • 49
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    The March 1981 Mount Etna eruption inferred through ground deformation modelling (1999)
    In:  Phys. Earth Plan. Int., Taipei, Elsevier, vol. 112, no. 1, pp. 125-136, pp. 2091, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Volcanology ; PEPI ; Modelling
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  • 50
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    The tensile dislocation problem in a layered elastic medium (1999)
    In:  Geophys. J. Int., Taipei, Elsevier, vol. 136, no. 2, pp. 341-356, pp. 2091, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: cracks and fractures (.NE. fracturing) ; Dislocation ; Modelling ; Layers ; rifting ; Elasticity ; Stress ; Inhomogeneity ; Volcanology ; GJI
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  • 51
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    Analysis of earthquake recordings obtained from the Seafloor Earthquake Measurement System (SEMS) instruments deployed off the coast of Southern California (1999)
    In:  Bulletin of the Seismological Society of America, Luxembourg, Conseil de l'Europe, vol. 89, no. 1, pp. 260-274, pp. L15S17, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: OBS ; Instruments ; Seismology ; Data analysis / ~ processing ; BSSA
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  • 52
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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)
    Details
    Publication Date: 1996
    Keywords: Site amplification ; Strong motions ; Finite difference method ; USA ; Waves ; Seismology ; accelerations ; topography ; BSSA
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  • 53
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    Stress drop and frictional heating during the 1994 deep Bolivia earthquake (1999)
    In:  Geophys. Res. Lett., Leipzig, Birkhäuser Verlag, vol. 26, no. 23, pp. 3521-3524, pp. 2366, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Stress drop ; Earthquake ; Geothermics ; 7209 ; Seismology ; Earthquake ; dynamics ; and ; mechanics ; 8130 ; Tectonophysics ; Heat ; generation ; and ; transport ; 8164 ; Stresses ; crust ; and ; lithosphere ; GRL
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  • 54
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    Clustering and size distributions of fault patterns: Theory and measurements (1999)
    In:  Geophys. Res. Lett., Leipzig, 3-4, vol. 26, no. 13, pp. 2001-2004, pp. L19606, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Pattern recognition ; Modelling ; Structural geology ; Fault zone ; GRL
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  • 55
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    Macintosh shareware/freeware earth science software (1999)
    In:  Computers and Geosciences, Hannover, FU Berlin, vol. 25, no. 4, pp. 335-340, pp. 5091692, (ISBN: 0-12-018847-3)
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    Publication Date: 1999
    Keywords: Data analysis / ~ processing ; Review article ; C&G
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  • 56
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    Staggered mesh for the anisotropic and viscoelastic wave equation (1999)
    In:  Geophysics, Luxembourg, Conseil de l'Europe, vol. 64, no. 6, pp. 1863-1866, pp. 1972, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Waves ; Synthetic seismograms ; Anisotropy ; Inelastic ; Rheology ; Elasticity
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  • 57
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    Rupture process of the 1995 Antofagasta subduction earthquake (Ms-2dwus0 = 8.1) (1999)
    In:  Pageoph, Luxembourg, Conseil de l'Europe, vol. 154, no. 3, pp. 677-708, pp. B04313, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Fracture ; Source ; Chile ; Tsunami(s) ; Subduction zone ; Seismicity ; Pageoph
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  • 58
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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)
    Details
    Publication Date: 1996
    Keywords: Borehole geophys. ; scientific drilling ; Vertical seismic profiling ; EUROPROBE (Geol. and Geophys. in eastern Europe) ; SG3
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  • 59
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    Visual basic programs for one, two, or three-dimensional geostatistical analysis (1998)
    In:  Computers and Geosciences, Luxembourg, Conseil de l'Europe, vol. 24, no. 6, pp. 531-536, pp. B04313, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1998
    Keywords: Statistical investigations ; Data analysis / ~ processing ; software ; C&G
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  • 60
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    Discriminating Ripple-fired explosions with high-frequency (〉16 Hz) data (1998)
    In:  Bull. Seism. Soc. of America, Luxembourg, Conseil de l'Europe, vol. 88, no. 4, pp. 963-972, pp. B04313, (ISBN: 0-12-018847-3)
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    Publication Date: 1998
    Keywords: High frequency ... ; Discrimination ; Seismology ; Source ; BSSA
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  • 61
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    What's next on the Internet (1998)
    In:  Computers and Geosciences, Luxembourg, Conseil de l'Europe, vol. 24, no. 7, pp. 627-632, pp. B04313, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1998
    Keywords: WWW ; teaching ; lecturing ; public ; outreach ; C&G
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  • 62
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    Ground motion modelling with a stochastically perturbed excitation (1999)
    In:  Journal of Seismology, Luxembourg, Conseil de l'Europe, vol. 3, no. 2, pp. 45-59, pp. B04313, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Modelling ; Strong motions ; Seismology ; Statistical investigations ; Zahradnik ; JOSE
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  • 63
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    Lateral propagation effects observed at Parkway, New Zealand. A case history to compare 1D versus 2D site effects (1999)
    In:  Bull. Seism. Soc. Am., Warszawa, Conseil de l'Europe, vol. 89, no. 3, pp. 718-732, pp. L12S07, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Seismology ; Wave propagation ; Strong motions ; Site amplification ; BSSA
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  • 64
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    Lateral propagation effects observed at Parkway, New Zealand. A case history to compare 1D versus 2D site effects (1999)
    In:  Bull. Seism. Soc. Am., Warszawa, Conseil de l'Europe, vol. 89, no. 3, pp. 718-732, pp. L12S07, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Wave propagation ; Site amplification ; Two-dimensional ; BSSA ; Chavez ; Garcia
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  • 65
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    Love waves in multilayered media with irregular interfaces: I. Modal solutions and excitation formulation (1999)
    In:  Bull. Seism. Soc. Am., Taipei, Elsevier, vol. 89, no. 6, pp. 1519-1534, pp. B09401, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Seismology ; Love-waves ; Synthetic seismograms ; NOModelling ; Inhomogeneity ; BSSA
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  • 66
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    On generalized plane strain poroelasticity (1998)
    In:  International Journal of Rock Mechanics and Mining Sciences, Taipei, Elsevier, vol. 35, no. 2, pp. 183-193, pp. B09401, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1998
    Keywords: Elasticity ; Rock mechanics ; Physical properties of rocks ; porosity
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  • 67
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    Multifractality and spatial statistics (1999)
    In:  Computers and Geosciences, Taipei, Elsevier, vol. 25, no. 9, pp. 949-961, pp. B09401, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: FractureT ; Statistical investigations ; C&G
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  • 68
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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)
    Details
    Publication Date: 1996
    Keywords: paleo ; Stress ; Geol. aspects ; Structural geology ; JSG
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  • 69
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    Development of intraformational (Oligocene-Miocene) faults in the northern North Sea: influence of remote stresses and doming of Fennoscandia (1999)
    In:  J. Struct. Geol., London, Institution of Mining and Metallurgy, vol. 21, no. 10, pp. 1457-1475, pp. 1869, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Tectonics ; Scandinavia ; Stress ; Fault zone ; Plate tectonics ; Structural geology ; JSG
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  • 70
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    Polarimetric SAR interferometry (1998)
    In:  IEEE Transactions on Geoscience and Remote Sensing, Heidelberg, Institution of Mining and Metallurgy, vol. 36, no. 5, pp. 1551-1565, pp. 2074, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1998
    Keywords: InSAR ; Geodesy ; Crustal deformation (cf. Earthquake precursor: deformation or strain)
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  • 71
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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)
    Details
    Publication Date: 1996
    Keywords: Seismicity ; Friction ; Seismology ; JGR
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  • 72
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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)
    Details
    Publication Date: 1996
    Keywords: Inelastic ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Earthquake ; JGR
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  • 73
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    Numerical models of crustal deformation in seismic zones (1999)
    In:  Advances Geophys., Heidelberg, Elsevier, vol. 41, no. 8, pp. 133-231, pp. 1516, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Modelling ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Seismicity ; ADG
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  • 74
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    Components of dynamic digital maps (1999)
    In:  Computers and Geosciences, Roma, Elsevier, vol. 25, no. 4, pp. 511-522, pp. 2099, (ISBN: 0-12-018847-3)
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    Publication Date: 1999
    Keywords: GIS ; Digital elevation model ; C&G
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  • 75
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    Non-double-couple microearthquakes in the geothermal field of Larderello, central Italy (1998)
    In:  Tectonophysics, Roma, Publicazioni dell'Istituto Nazionale di Geofisica, vol. 289, no. 1-3, pp. 203-220, pp. 2099, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1998
    Keywords: Induced seismicity ; Seismicity ; Geothermics ; Fault plane solution, focal mechanism ; extension ; explosion ; Stress
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  • 76
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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)
    Details
    Publication Date: 1996
    Keywords: Anisotropy ; Local earthquakes ; Borehole geophys. ; USA ; Seismic arrays ; Seismology ; anisotropy ; southern ; California ; BSSA
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  • 77
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    Dedication to Daniel F. Merriam (1999)
    In:  Computers and Geosciences, Bonn, Hungarian Academy of Science, vol. 25, no. 4, pp. 315-318, pp. B04102, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Data analysis / ~ processing ; Review article ; C&G
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  • 78
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    Refined coseismic displacement modeling for the 1994 Shikotan and Sanriku-Oki earthquakes (1998)
    In:  Geophys. Res. Lett., Bonn, Hungarian Academy of Science, vol. 25, no. 17, pp. 3219-3222, pp. B04102, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1998
    Keywords: Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Earthquake ; Global Positioning System ; 7209 ; Seismology ; Earthquake ; dynamics ; and ; mechanics ; GRL ; 1242 ; Geodesy ; and ; gravity ; Seismic ; deformations ; (7205) ; 1243 ; Space ; geodetic ; surveys
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  • 79
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    Go-ahead for San Andreas drilling project ... (1999)
    In:  Nature, Warszawa, Pergamon, vol. 401, no. 6748, pp. 5, pp. B06311, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Project report/description ; Stress ; SAF ; Fault zone ; ICDP
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  • 80
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    Crustal structure above the Iceland mantle plume imaged by the ICEMELT refraction profile (1998)
    In:  Geophys. J. Int., Warszawa, Pergamon, vol. 135, no. 3, pp. 1131-1149, pp. B05310, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1998
    Keywords: Velocity depth profile ; Refraction seismics ; Earth model, also for more shallow analyses ! ; Flovenz ; GJI
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  • 81
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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)
    Details
    Publication Date: 1996
    Keywords: Inversion ; Fracture ; Source
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  • 82
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    The effects of image misregistration on the accuracy of remotely sensed change detection (1998)
    In:  IEEE Transactions on Geoscience and Remote Sensing, Warszawa, Pergamon, vol. 36, no. 5, pp. 1566-1577, pp. L19306, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1998
    Keywords: Pattern recognition ; NOISE ; Data analysis / ~ processing ; Error analysis
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  • 83
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    A semi-empirical method for simulating strong ground motions based on variable-slip rupture models for large earthquakes (1999)
    In:  Bulletin of the Seismological Society of America, Warszawa, Pergamon, vol. 89, no. 1, pp. 36-53, pp. B06311, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Strong motions ; Synthetic seismograms ; Modelling ; Fracture ; SModelling ; BSSA
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  • 84
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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)
    Details
    Publication Date: 1996
    Keywords: Fracture ; Source ; Seismology ; JGR
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  • 85
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    Vibroseis recording techniques and data reduction from the Jemez tomography experiment (1999)
    In:  Bull. Seism. Soc. Am., Warszawa, Army Corps of Engineers, Woodward-Clyde Consultants, vol. 89, no. 5, pp. 1352-1365, pp. 1013, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Seismics (controlled source seismology) ; Tomography ; BSSA
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  • 86
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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)
    Details
    Publication Date: 1996
    Keywords: Modelling ; Boundary Element Method ; Elasticity
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  • 87
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    Experiments and simulations track crack propagation in silicon wafers (1999)
    In:  Phys. Today, London, Army Corps of Engineers, Woodward-Clyde Consultants, vol. 52, no. 2, pp. 17-18, pp. 1013, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Fracture ; cracks and fractures (.NE. fracturing) ; solid ; state ; physics ; Mineralogy ; Rock mechanics
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  • 88
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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)
    Details
    Publication Date: 1996
    Keywords: Site amplification ; Modelling ; SH waves ; noksp ; BSSA
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  • 89
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    Dynamic stress changes during earthquake rupture (1998)
    In:  Bull. Seism. Soc. of America, London, Army Corps of Engineers, Woodward-Clyde Consultants, vol. 88, no. 2, pp. 512-522, pp. 1013, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1998
    Keywords: Seismology ; Stress drop ; Fracture ; Source ; BSSA
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  • 90
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    The lithospheric structure and evolution of the Pannonian/Carpathian/Dinaride region (1999)
    In:  Tectonophysics, London, Army Corps of Engineers, Woodward-Clyde Consultants, vol. 297, no. 1-4, pp. 1-293, pp. 1062, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: EUROPROBE (Geol. and Geophys. in eastern Europe) ; Earth model, also for more shallow analyses ! ; Velocity depth profile ; Deep seismic sounding (espec. cont. crust) ; Geol. aspects
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  • 91
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    Empirical Green's Functions: A comparison between pulse width measurements and deconvolution by spectral division (1999)
    In:  Bulletin of the Seismological Society of America, London, Army Corps of Engineers, Woodward-Clyde Consultants, vol. 89, no. 1, pp. 178-189, pp. 1062, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Deconvolution ; Spectrum ; Seismology ; BSSA
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  • 92
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    Origin, effects of Mayasa volcano's continued unrest probed in Nicaragua (1999)
    In:  Eos, Trans., Am. Geophys. Un., London, Army Corps of Engineers, Woodward-Clyde Consultants, vol. 80, no. 48, pp. 575, 579, 581, pp. 1062, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Project report/description ; Volcanology ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Global Positioning System ; Gravimetry, Gravitation ; Geochemistry ; microgravity ; changes ; no ; deformation ; gas ; sulfur
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  • 93
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    Focal mechanism determination and identification of the fault plane of earthquakes using only one or two near-source seismic recordings (1999)
    In:  Bull. Seism. Soc. Am., London, Army Corps of Engineers, Woodward-Clyde Consultants, vol. 89, no. 6, pp. 1558-1574, pp. 1062, (ISBN: 0-12-018847-3)
    Details
    Publication Date: 1999
    Keywords: Seismology ; Fault plane solution, focal mechanism ; Nearfield ; Data analysis / ~ processing ; BSSA
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  • 94
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    An intensity survey of households affected by the Northridge, California, earthquake of 17 January 1994 (1998)
    In:  Bull. Seism. Soc. of America, London, 416 pp., Geological Society, vol. 88, no. 2, pp. 441-462, pp. L18607, (ISBN 1-86239-117-3)
    Details
    Publication Date: 1998
    Keywords: Intensity ; Earthquake ; Earthquake risk ; BSSA
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  • 95
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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)
    Details
    Publication Date: 1996
    Keywords: Stress ; Geol. aspects ; Physical properties of rocks ; Fracture
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  • 96
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    The geomorphology and sedimentology of the July 9th 1956 Aegean Sea tsunami (1999)
    Elsevier
    In:  Marine Geology (Internat. J. of Marine Geol., Geochem. and Geophys.), Amsterdam, Elsevier, vol. 21, no. 1, pp. 83-96, pp. 2486, (ISBN 1-86239-117-3)
    Details
    Publication Date: 1999
    Keywords: Tsunami(s) ; Geol. aspects
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  • 97
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    Upper plate deformation associated with seamount subduction (1998)
    In:  Tectonophys., Amsterdam, Elsevier, vol. 293, no. 3-4, pp. 207-224, pp. 2486, (ISBN 1-86239-117-3)
    Details
    Publication Date: 1998
    Keywords: Subduction zone ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Plate tectonics ; Hune ; Huene
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  • 98
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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)
    Details
    Publication Date: 1996
    Keywords: Tectonics ; metamorphic ; China ; scientific drilling ; Geol. aspects
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  • 99
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    Global Positioning System observations of fault afterslip and upper crustal deformation following the Northridge earthquake (1998)
    In:  Journal of Geophysical Research, Amsterdam, Elsevier, vol. 103, no. B9, pp. 21285-21297, pp. 2083, (ISBN 1-86239-117-3)
    Details
    Publication Date: 1998
    Keywords: Geodesy ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; Earthquake ; postseismic ; JGR
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  • 100
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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)
    Details
    Publication Date: 1996
    Keywords: Tomography ; Fault zone ; triple ; junction ; Modelling ; Crustal deformation (cf. Earthquake precursor: deformation or strain) ; JGR
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