Fossil Earthquakes: The Formation and Preservation of Pseudotachylytes [electronic resource] / by Aiming Lin.

Por: Lin, Aiming [author.]Tipo de material: TextoTextoSeries Lecture Notes in Earth Sciences, 111Editor: Berlin, Heidelberg : Springer Berlin Heidelberg, 2008Descripción: XII, 348 p. online resourceTipo de contenido: text Tipo de medio: computer Tipo de portador: online resourceISBN: 9783540742364Trabajos contenidos: SpringerLink (Online service)Tema(s): Geology | Geology, Structural | Physical geography | Mineralogy | Geosciences | Geology | Structural Geology | Geophysics/Geodesy | MineralogyFormatos físicos adicionales: Sin títuloClasificación CDD: 551 Clasificación LoC:QE1-996.5Recursos en línea: de clik aquí para ver el libro electrónico
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Springer eBooksResumen: The topics covered in this book encompass the principl results of field investigations, analyses of meso-scale and micro-scale textures and structures, laboratory experiments, chemical analyses, conceptual fault models, as well as the implications of fault related pseudotachylyte an its related fault rocks for our understanding of earthquakes. We hope that this book helps to bridge the gap between seismology and geology and that it encourages further studies of earthquake and seismic faulting processes.
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Terminology and Origin of Pseudotachylyte -- Pseudotachylyte-Related Fault Rocks and Conceptual Fault Models -- Tectonic Environment and Structure of Pseudotachylyte Veins -- Pseudotachylyte Matrix -- Microlites -- Fragments Within Pseudotachylyte Veins -- Chemical Composition and Melting Processes of Pseudotachylyte -- Formation of Pseudotachylyte in the Brittle and Plastic Regimes -- Crushing-Origin Pseudotachylyte and Veinlet Cataclastic Rocks -- Landslide-related Pseudotachylyte -- Experimentally Generated Pseudotachylyte.

The topics covered in this book encompass the principl results of field investigations, analyses of meso-scale and micro-scale textures and structures, laboratory experiments, chemical analyses, conceptual fault models, as well as the implications of fault related pseudotachylyte an its related fault rocks for our understanding of earthquakes. We hope that this book helps to bridge the gap between seismology and geology and that it encourages further studies of earthquake and seismic faulting processes.

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