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Fossil Earthquakes: The Formation and Preservation of Pseudotachylytes de Aiming Lin

Fossil Earthquakes: The Formation and Preservation of Pseudotachylytes: Lecture Notes in Earth Sciences, cartea 111

Autor Aiming Lin
en Limba Engleză Hardback – 22 noi 2007

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Specificații

ISBN-13: 9783540742357
ISBN-10: 3540742352
Pagini: 350
Ilustrații: XII, 348 p.
Dimensiuni: 155 x 235 x 19 mm
Greutate: 0.61 kg
Ediția:2008
Editura: Springer Berlin, Heidelberg
Colecția Springer
Seria Lecture Notes in Earth Sciences

Locul publicării:Berlin, Heidelberg, Germany

Public țintă

Research

Cuprins

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.

Recenzii

From the reviews:
"The book by Professor Lin provides an overview of the current understanding of fault-related pseudotachylytes. The overview is based on a comprehensive examination of the literature and on the experience of the author … . It will be helpful for students and researchers involved in the new era of pseudotachylyte research, which relies more and more on high-velocity friction experiments." (Olivier Fabbri, The Journal of Geology, Vol. 116, 2008)

Textul de pe ultima copertă

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.