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The Seismic Cycle
The study of the seismic cycle has many applications, from the study of faulting to the estimation of seismic hazards. It must be considered at different timescales, from that of an earthquake, the co-seismic phase (a few seconds), the post seismic phase (from months to dozens of years) and the inter-seismic phase (from dozens to hundreds of years), up to cumulative deformations due to several seismic cycles (from a few thousand to hundreds of thousands of years). The Seismic Cycle uses many different tools to approach its subject matter, from short-term geodesic, such as GPS and InSAR, and seismological observations to long-term tectonic, geomorphological, morphotectonic observations, including those related to paleoseismology. Various modeling tools such as analog experiences, experimental approaches and mechanical modeling are also examined. Different tectonic contexts are considered when engaging with the seismic cycle, from continental strike-slip faults to subduction zones such as the Chilean, Mexican and Ecuadorian zones. The interactions between the seismic cycle and magmatism in rifts and interactions with erosion in mountain chains are also discussed.
Best Practices in Physics-based Fault Rupture Models for Seismic Hazard Assessment of Nuclear Installations
This volume collects several extended articles from the first workshop on Best Practices in Physics-based Fault Rupture Models for Seismic Hazard Assessment of Nuclear Installations (BestPSHANI). Held in 2015, the workshop was organized by the IAEA to disseminate the use of physics-based fault-rupture models for ground motion prediction in seismic hazard assessments (SHA). The book also presents a number of new contributions on topics ranging from the seismological aspects of earthquake cycle simulations for source scaling evaluation, seismic source characterization, source inversion and physics-based ground motion modeling to engineering applications of simulated ground motion for the analy...
Mountain Building
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Individuation and Attachment in the Works of Isabelle de Charrière
The novels published by Isabelle de Charrière before the French Revolution offer a perceptive account of the psychology and the social climate of the late eighteenth century. The anti-Freudian psychoanalysis of the neurologist and psychiatrist Heinz Kohut (1913-81) is used in this study as a means of developing an awareness of the position of the fictional characters. Feminist and Freudian readings of Charrière's novels of the 1780s have stressed the 'closed' deterministic atmosphere of contemporary society; this new study emphasises what can be called the 'modern' side of the novels: patriarchal society and individual needs confront each other and allow the relationships to be seen in a new light. By means of Kohut's notion of 'selfobject' a rich insight is gained into the complex relationships described by Isabelle de Charrière.
Trauma and Its Representations
Mimesis has been addressed frequently in terms of literary or visual representation, in which the work of art mirrors, or fails to mirror, life. Most often, mimesis has been critiqued as a simple attempt to bridge the distance between reality and its representations. In Trauma and Its Representations: The Social Life of Mimesis in Post-Revolutionary France, Deborah Jenson argues instead that mimesis not only denotes the representation of reality but is also a crucial concept for understanding the production of social meaning within specific historical contexts. Examining the idea of mimesis in the French Revolution and post-Revolutionary Romanticism, Jenson builds on recent work in trauma studies to develop her own notion of traumatic mimesis. Through innovative readings of museum catalogs, the writings of Benjamin Constant, the novels of George Sand and Gustave Flaubert, and other works, Jenson demonstrates how mimesis functions as a form of symbolic wounding in French Romanticism.
Marine Boilers
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The Afar Volcanic Province Within the East African Rift System
The seismically and volcanically active East African Rift System is an ideal laboratory for continental break-up processes: it encompasses all stages of rift development. Its northernmost sectors within the Afar volcanic province include failed rifts, nascent sea-floor spreading, and youthful passive continental margins associated with one or more mantle plumes. A number of models have been proposed to explain the success and failure of continental rift zones, but there remains no consensus on how strain localizes to achieve rupture of initially 125-250 km-thick plates, or on the interaction between the plates and asthenospheric processes. This collection of papers provides new structural, stratigraphic, geochemical and geophysical data and numerical models needed to resolve fundamental questions concerning continental break-up and mantle plume processes. The focus is on how mantle melt intrudes and is distributed through the plate, and how this magma intrusion process controls along-axis segmentation and facilitates break-up.
Le cycle sismique
Les séismes sont parmi les manifestations les plus destructrices de la dynamique interne de la Terre. Cet ouvrage analyse le cycle sismique à différentes échelles de temps : le séisme (quelques secondes), les phases post-sismique (quelques années à dizaines d’années) et inter-sismique (quelques dizaines à centaines d’années), et enfin la déformation cumulée due à plusieurs cycles sismiques (quelques milliers à centaines de milliers d’années). Le cycle sismique est ici étudié à travers des observations court terme sismologiques et géodésiques (GPS et InSAR) et des observations long terme tectoniques, géomorphologiques, morphotectoniques et paléosismologiques. Divers outils de modélisation sont présentés : les expériences analogiques, les approches expérimentales et la modélisation cinématique ou mécanique. Le cycle sismique est illustré dans différents contextes tectoniques, des failles décrochantes continentales aux zones de subduction. Enfin, les interactions entre le cycle sismique et le magmatisme dans les rifts ainsi que les interactions avec l’érosion dans les chaînes de montagnes sont également traitées.
