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71.
72.
Prof. Dr. Gerhard Keller 《International Journal of Earth Sciences》1968,57(2):445-454
Zusammenfassung In Bohuslän an der schwedischen Skagerrak-Küste befinden sich bei Lysekil Rundhöcker, die aus klüftigem Granit bestehen. Das Gefügeinventar ist sehr umfangreich, doch fällt eine Hauptrichtung auf, welche die Eisbewegung steuerte. Außer den tektonischen Klüften tritt die Entspannungsklüftung in ihrer typischen Art insofern auf, als sie morphoparallel ist und die Außenform der Rundhöcker nachbildet. Durch das Vorhandensein einer Diskordanz zwischen der Aufgleitfläche des Eises und den Entspannungsflächen im Granit ist über das Alter der Rundhöcker auszusagen, daß ihre Anlage älter als die Eisbedeckung ist. Das Eis benutzte die Entspannungsflächen teilweise als Bewegungsbahn oder kappte sie. Das Alter der Rundhöcker und ihre räumliche Anordnung wird daher präglazial sein und ist in das Tertiär zu stellen. Die vorgefundenen älteren Formen überprägte das Eis oft am stärksten auf der Leeseite und schuf dann steilwandige Nischen mit ortsfremden Findlingen als Inhalt.
In the Bohuslän District, on the Swedish Skagerrak coast, humps may be found near Lysekil, which consist of jointed granite. The fabric is very comprehensive, but there is one main direction guiding the ice movement. Besides these joints, there are relaxation planes in their typical formations; they run parallel to the morphology and re-shape the exterior forms of the humps.The presence of a discordance between the gliding surface and the relaxation planes in the granite determines the age of the humps, i. e., their origin is older than the ice cover. The ice made use of these planes by moving on or by cutting them. The age of the humps and their arrangement in space should, therefore, be preglacial and be assigned to the tertiary. The older forms encountered re-formed the ice most strongly on the leeward side, and there are precipitous niches containing erratic blocks.
Résumé A Bohuslän sur la côte suédoise de Skagerrak se trouvent à côté de Lysekil des roches moutonnées, formées de granit diaclase. La structure en question est très riche, mais une direction principale se distingue, celle qui réglait le mouvement glaciaire. Apart les diaclases intervient une diaclase de relaxation dans sa forme typique aussi loin qu'elle est morphoparallèle et qu'elle imite la forme extérieure des roches moutonnées. A travers l'existence d'une discordance mécanique entre la surface de glissement du glacier et les surfaces de relaxation dans le granit peut on déterminer l'âge des roches moutonnées, que leur formation est plus vieille que celle de la couverture glaciaire. Le glacier utilisait les surfaces de relaxation comme voie de déplacement, ou bien il les coupait. C'est pour cela que l'âge des roches moutonnées et leur disposition dans l'éspace est préglacial, et est à ranger dans l'ère tertiaire. Le glacier influença les anciennes formes trouvées, souvent le plus fort sur le côté sous le vent, et fit des nids à falaises abruptes contenant des blocs erratiques venant d'autre part.
Lysekil (Bohuslän, ) . , , . , , . , . . , -- . .相似文献
73.
Gerhard H. Eisbacher 《International Journal of Earth Sciences》1973,62(1):29-53
Zusammenfassung Die Orientierung von post-orogenen Klüften in proterozoischen Sedimentgesteinen des Elliot Lake-Gebietes, Canada, läßt sich mit der meßbaren Gesteinsentspannung in Bohrlöchern in Beziehung bringen. Steile lokale und regionale Kluftscharen ohne Bewegungsspuren streichen in Richtung der elastischen Hauptentformungsachse, also in Richtung der größten in-situ-Kompressionsspannung.Die Klüfte lassen sich deshalb wahrscheinlich als Extensionsfugen erklären, und zwar als Resultat der Wechselwirkung zwischen Oberflächenabtrag des Gesteins und remanenter tektonischer Gesteinsspannung. Der vorgeschlagene Mechanismus sollte auch zum Verständnis von spät-orogenen (ac)-Klüften in gefaltetem Deckgebirge und oberflächenparallelen Klüften in massigen Gesteinen beitragen.
Orientation of post-orogenic joints in Proterozoic sedimentary rocks of the Elliot Lake area (Canada) seems to be directly related to elastic-strain-recovery as measured in boreholes. Steep local and regional joint sets without displacement are parallel with the axis of maximum elastic-strain-recovery (i. e. the direction of the major principal in situ stress component). Consequently these joints are interpreted as extension joints forming as a result of the interaction between natural (or artificial) erosion of the rock mass and its remanent tectonic stresses. The proposed mechanism should also help to understand late-orogenic (ac)-joints in folded cover rocks and exfoliation joints in otherwise unjointed rocks.
Résumé L'orientation des diaclases post-tectoniques dans des roches sédimentaires protérozoïques de la région du Lac d'Elliot, Canada, peut être mise en relation avec les tensions élastiques des roches telles qu'on peut les mesurer dans les trous de forage. Les systèmes de diaclases redressées, locales et régionales, sans traces de mouvement, sont dirigés parallèlement aux axes principaux de la déformation élastique, c'est-à-dire à la direction de la plus grande compression in situ mesurée par le changement de forme d'un trou de sonde. Par conséquent, les diaclases s'expliquent vraisemblablement comme joints d'extension, et en fait comme le résultat de l'action réciproque entre des tensions tectoniques rémanentes et l'érosion en surface. Le mécanisme proposé explique aussi les diaclase (ac) tardives dans les couvertures plissées et l'exfoliation parallèle à la surface dans les roches massives.
- Elliot Lake, , . , in situ. , , , , , . - .相似文献
74.
Summary Simultaneous measurements of the electrical conductivity of air inside and outside of buildings have been performed with continuously recording electronic instruments of high sensitivity and short time constant. It appears that the electrical conductivity, a measure of the natural ionization of air, is one atmospheric-electric parameter that can manifest itself inside occupied buildings without appreciable difference in physical character from outside values.The probable importance of these experimental results for the field of bioclimatology is pointed out and the possibility is discussed that the electrical conductivity of air might be one of the searched—for parameters in associating physiological phenomena with weather changes.
With 1 Figure.
Publication No. 25 of the Institute of Geophysics, University of California at Los Angeles. The research reported in this paper has been sponsored in part by the Geophysics Research Directorate of the Air Force Cambridge Research Center, Air Research and Development Command, under Contract No. AF 19(122)-254. 相似文献
Zusammenfassung Gleichzeitige Messungen der luftelektrischen Leitfähigkeit im Freien und innerhalb von Gebäuden wurden mit kontinuierlich registrierenden Röhreninstrumenten von großer Empfindlichkeit und kurzer Zeitkonstante durchgeführt. Es wurde gefunden, daß die Leitfähigkeit als Maß der natürlichen Luftionisierung eine luftelektrische Größe darstellt, die ohne wesentliche physikalische Beeinflussung in bewohnte Gebäude einzudringen vermag.Die mögliche Bedeutung dieser experimentellen Ergebnisse für das Gebiet der Bioklimatologie wird angedeutet und die Wahrscheinlichkeit diskutiert, daß die luftelektrische Leitfähigkeit einen der noch unbestimmten Faktoren des Zusammenhanges physiologischer Erscheinungen mit Wetterveränderungen darstellen könnte.
Résumé Des instruments électroniques à enregistrement continu de haute fidelité et ayant une constante de courte durée ont permis de prendre des mesures simultanées de la conductivité électrique de l'air à l'intérieur et à l'extérieur de bâtiments. Il semble que la conductivité électrique, mesure de l'ionisation naturelle de l'air, soit un paramètre de l'électricité atmosphérique qui peut se manifester à l'intérieur de bâtiments habités sans différence appréciable de caractéristiques physiques avec celles des valeurs extérieures.L'importance probable de ces résultats expérimentaux dans le champ de la bioclimatologie est indiquée, et la possibilité que la conductivité atmosphérique puisse être un des paramètres recherchés dans l'association des phénomènes physiologiques avec des changements du temps est étudiée.
With 1 Figure.
Publication No. 25 of the Institute of Geophysics, University of California at Los Angeles. The research reported in this paper has been sponsored in part by the Geophysics Research Directorate of the Air Force Cambridge Research Center, Air Research and Development Command, under Contract No. AF 19(122)-254. 相似文献
75.
Gerhard Hahn Claes-Ingvar Lagerkvist 《Celestial Mechanics and Dynamical Astronomy》1987,43(1-4):285-302
Numerical integrations of 26 orbits of planet-crossing astetoids of Apollo-Amor type have been performed, in a solar system model including the perturbations by the planets from Venus to Neptune. The 15:th order RADAU integrator (Everhart, 1985) has been used. Orbits for the asteroids 433 Eros, 887 Alinda, 1036 Ganymed, 1221 Amor, 1580 Betulia, 1627 Ivar, 1685 Toro, 1862 Apollo, 1863 Antinous, 1864 Daedalus, 1865 Cerberus, 1915 Quetzalcoatl and 1916 Boreas have been integrated over 100 000 years forward in time and for 1866 Sisyphus, 2102 Tantalus, 2201 Oljato, 2329 Orthos, 3360 1981 VA, 3552 1983 SA, 1981 EJ30, 1985 PA, 1985 WA, 1986 DA 1986 JK and 1986 RA a period of about 33 000 years has been covered. The orbital evolutions of these asteroids are discussed. This work is part of a larger study of the long-term orbital evolution of planet-crossing asteroids and will be continued within the project SPACEGUARD (Milani et al., 1987). 相似文献
76.
Wolf Tietze Gerhard Kortum W. R. Mead T. K. Poiker C. Paddick George Kish A. Njøs H. Mensching V. Haarmann Uzo M. Igbozurike M. M. Yoshino Mushtaqur Rahman Lage Wahlström J. Connell Kazimierz Dziewonski Wayland R. Swain J. Humlum G. W. Lüttig Haruko Kishimoto Mai Britt E. Mørk 《GeoJournal》1982,6(3):270-280
77.
It is shown that endogenic lava flow processes can be identified by their characteristic effects on lunar crater size distributions without necessarily being able to recognise individual flows on the photographs studied. The thickness of lava flows or a series of flows can be estimated from these crater size distribution characteristics. The lava flow histories of the Apollo landing sites 11, 12 and 15 are discussed in detail. The thicknesses of the most recent (3–3.4 × 109 years ago) flows there and of the youngest flows in an area in south-west Mare Imbrium (3 × 109 years) are found to range between 30 and 60 m. The subsequent flow episodes at the landing sites showing up in the crater size distributions can be related to differences in the radiometric ages of the respective lunar rocks. 相似文献
78.
Matthias?AuerEmail author Gerhard?H.?Eisbacher 《International Journal of Earth Sciences》2003,92(2):210-227
The Northern Calcareous Alps (NCA) of southern Bavaria and northern Tyrol constitute a carbonate-dominated polyphase fold-thrust wedge; together with its Grauwacken Zone Basement, it is the northernmost part of the far-travelled Upper Austroalpine thrust complex of the Eastern Alps. The present geometry developed in several kinematic stages. Jurassic extensional faults that affected large parts of the NCA and their basement originated when the main part of the NCA was still located southeast of the Central Alpine Ötztal-Silvretta complex. These faults and related facies transitions influenced the later style of detachment of the NCA thrust sheets. Mid to Late Cretaceous detachment, thrust-sheet stacking and motion over the Central Alpine complex are registered in clastic deposits of syntectonic basins. The latest Cretaceous to Cenozoic NNE- to N-directed motion of the NCA towards Europe in front of the Central Alpine complex created another set of significant contraction structures, which at depth overprinted all previous structures. During Cretaceous to Cenozoic deformation, the NCA experienced about 80 km of shortening, i.e., about 73% along the TRANSALP Profile. The European basement and autochthonous Mesozoic cover beneath the allochthonous NCA thrust sheets and flysch complexes seem to have remained relatively undeformed. 相似文献
79.
Gerhard?SchmiedlEmail author Maria?Scherbacher Angela?A.?Bruch Bogomir?Jelen James?H.?Nebelsick Christoph?Hemleben Volker?Mosbrugger Helena?Rifelj 《International Journal of Earth Sciences》2002,91(1):123-132
Several sections from the uppermost Eocene and Oligocene of northern Slovenia have been investigated with respect to sedimentary facies, foraminiferal assemblages, stable isotopes, carbonate microfacies, and palynology. The main objective was to reconstruct the paleoenvironmental history of the Paleogene Paratethys in this region of the eastern Alpine realm. The sediments exhibit a transgressive succession beginning with conglomerates, sandstones, and mudstones of fluvial and lacustrine origin followed by carbonates and muddy marls indicating marine conditions. The foraminiferal faunal changes from brackish to shallow marine to deeper marine assemblages and the distribution of the palynofloras corroborate the sedimentological results. Microfacies analysis of the limestones shows a wide variation of shallow water, generally mud-rich facies dominated by coralline algae, foraminifera, and corals. Microfaunas adapted to low-oxygen conditions indicate temporal sluggish bottom-water circulation which can be associated with high fresh-water fluxes. These results are discussed as reflecting both the global sea-level rise during the Early Oligocene and the regional tectonic and climatic evolution. 相似文献
80.
Pleistocene tectonics inferred from fluvial terraces of the northern Upper Rhine Graben, Germany 总被引:1,自引:0,他引:1
This study of fluvial terraces of the River Rhine and tributaries aims to search for indications of Pleistocene tectonic activity. The study area includes the northern Upper Rhine Graben (URG), the Mainz Basin and the adjacent Rhenish Massif with the Middle Rhine Valley. High rates of Quaternary surface processes, large amount of human modifications, relatively slow tectonic deformation and presently low intra-plate seismic activity characterize this area. Therefore, the records of relatively slow tectonic deformation are less well preserved and thus difficult to detect. This study uses the relative position of fluvial terraces to determine the more local effects of fault movements on the terraces and to evaluate their displacement rates and patterns. The research is based on a review of previous terrace studies and new terrace mapping from the eastern Mainz Basin and the bordering URG using topographic map interpretations and field observations. This newly mapped sequence of terrace surfaces can be correlated to other terraces in the vicinity on the basis of relative height levels. Terrace correlation between the western Mainz Basin and Middle Rhine Valley relies on a single chronostratigraphic unit (Mosbach sands) and additional relative height correlations. This is the first study to present a continuous correlation of terraces from the western margin of the URG to the Rhenish Massif and enables the study of the transition from the subsiding graben to the uplifted Rhenish Massif. By means of a longitudinal profile, which ranges from the URG to the Rhenish Massif, the influence of individual fault movements on the terrace levels and the large-scale regional uplift is demonstrated. It is evident from the profile that the uplift of Early to Middle Pleistocene terraces increases northwards, towards the Rhenish Massif. The uplift was diachronic, with a significant pulse occurring first in the northern URG (Lower Pleistocene) and later in the Rhenish Massif (Middle Pleistocene). The largest vertical displacements are recorded for the boundary fault separating the Mainz Basin and the Rhenish Massif (Hunsrück–Taunus Boundary Fault) and for faults bounding the northeastern Mainz Basin. The motions and displacement rates calculated for individual faults indicate deformation rates in the order of 0.01–0.08 mm/year. At this stage, the calculation of displacement rates depends mostly on a single dated stratigraphic unit. Additional dating of terrace deposits is urgently needed to better constrain the temporal development of the terrace sequence and the impact of tectonic movements. 相似文献