Erdol-Erdgas-Geologie und Plattentektonik. (Oil and gas geology and plate tectonic)
Several processes of oil and gas geology are studied in connection with plate-tectonical processes. Thus it becomes clear, that there is a distinct difference between the Paleozoic development of the Europian plate and the Mesozoic development. (HL).
Earthquakes and plate tectonics in The Earth: its origin, structure and evolution.
In this review of observations and hypotheses pertinent to earthquake occurence, emphasis is placed on major earthquakes at non-accretionary plate margins because these events account for nearly all seismically related slip. Among the more topical
problems given at least brief mention are possible relationships between global seismicity and plate dynamics, stress drops and apparent stress from earthquakes, tectonic stress near plate margins and within the plates, and mechanical properties of the slip
Conditions pour faire la distinction entre plate-forme littorale et falaises plongeantes et entre plate-forme inclinée sans rupture topographique et plate-forme horizontale limitée vers la mer par un plan de forte inclinaison, l'A. examine les
Geomorphology of the central Southern Alps, New Zealand : the interaction of plate collision and atmospheric circulation in The geomorphology of plate boundaries and active continental margins.
, produced by plate convergence, and global atmospheric circulation.
Tectonic geomorphology of the Hikurangi margin : surface manifestations of different modes of subduction in The geomorphology of plate boundaries and active continental margins.
is present. These differences manifest greater and lesser degrees of coupling of the two plates (oceanic Pacific plate and continental Australia plate) in the southern and northern regions, respectively.
Plate boundary tectonics and oceanic island geomorphology in The geomorphology of plate boundaries and active continental margins.
This paper illustrates how studies of the geomorphology of oceanic islands can contribute to the understanding of nearby plate boundaries. For this purpose, an oceanic island is defined as one within an ocean basin. Case studies are given of three
O periodicnosti kolebatel'nyh dvizenij Sibirskoj platformy i ih sravnenie s razvitiem Vostocno-Evropejskoj platformy. (Sur la périodicité des mouvements oscillatoires de la plate-forme sibérienne et leur comparaison avec le développement de la plate
Europe ; Géographie physique ; Mouvement oscillatoire ; Plate-forme ; Périodicité ; Sibir' ; Tectonique ; URSS d'Asie
La morphogenèse des plates-formes de corrosion littorale dans les grès calcaires (plates-formes supérieure et plates-formes à vasques) et le problème des vasques d'après des observations faites à Madagascar
Après quelques considérations d'ensemble sur les plates-formes et leur origine, les AA. traitent globalement les facteurs exogènes de la lithogenèse et les facteurs paléogéographiques, avant d'adopter un plan zonal (chapitres 5 à 8). Les derniers
chapitres abordent des phénomènes plus précis : les avant-deltas, les plates-formes des mers à marée, les types morphologiques de plates-formes et les minerais utiles de leurs sédiments. - (FC)
Vertical movement of isolated oceanic islands at plate margins : evidence from emergent reefs in Tonga (Pacific Ocean), Cayman Islands (Caribbean Sea) and Christmas Island (Indian Ocean) in The geomorphology of plate boundaries and active
This paper examines the evidence for vertical movement of oceanic islands at three plate margin locations. Each is located adjacent to a deep ocean trench, but represents a different plate margin setting from a different ocean. For each of the areas