دانشجويان و دانش‌آموختگان زمين‌شناسي

Many faults appear to form persistent zones of weakness that fundamentally influence the distribution, architecture and movement patterns of crustal-scale deformation and associated process in both continental and oceanic regions. This book brings together papers by an international group of Earth Scientists to discuss a broad range of topics centred upon the controls of fault weakening and the role of such faults during lithosphere deformation. Readership:Academic structural-tectonic geologists, microstructural geologists, rheologists, geophysicists and people studying geodynamics. Also, petroleum geologists, hardrock geologists, mining geologists, hydrogeologists and metamorphic geologists. Suitable for postgraduate students.

344 pages.

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The Nature and Tectonic Significance of Fault Zone Weakening (29.2 Mb)